Compilation géologique de l'Orogène de l'Ungavamern.gouv.qc.ca/publications/mines/quebec-minier/orogene_ungava.… · NAR3 Monzogranite + syénogranite avec biotite ± hornblende;
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#
&<
&<&<
&<&<#
#&<
&<
#
&<
&<
&<#
##
#
&<
&<
&<
#@A
#@A
&<
@A @A
@A
#
#
#
@A#
#
#
&<
&<
&<
&<
#
#
#
#
##
#
#
#
@A#
#
#
#
&<
&<
#
#
@A&<
#
#
#
#
#
#
#
&<
@A
@A
&<
##
B
B
@A
#
#
&< &<
#
&<
&<
#
#&<
#
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#
#
#
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&<
#
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#
#
I3B
I3B
I3B
I3B
I3B
I3B I3B
I3B
I3B
I3B
I3B
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=ble
=ble=ble
=ble
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=ble
!lrd1
!fth1
!lrd1
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!fth1
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=ble
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=ble =ble=ble
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!lep
=ble
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=ble =ble
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?pra
=ktz
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=ble
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=ble
=ble =ble
=ble
=ble
?kuv
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=ble =ble=ble
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=pay=pay =pay
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!nan
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=ble
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2fra=ble
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!nan
2fra
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!byl1
=pay
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=pay
=ble
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=ble
=ble
=ble
=ktz
!nan
!nan
=pay
=ktz ?pra
=ktz
!lsd
=ktz
=ble
2fra
2fra
!nan
=pay
=pay
=pay
=pay
=pay
=pay
=pay
=pay
=pay=pay
=pay
=pay
!kmb
=pay
=pay
=pay
=pay
!nan
=pay
=ble
!jut1
=ble=ble
=ble =ble
=pay
=ble
=ble
=ktz
=ktz
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=ble
=sp1
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=ble
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=ble
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?pra
=ble
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=ktz
!lep
=ble
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!lep
=ble
!nan
=ktz
2fra
!KOV4
!lep
=ni
!lep
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=pay
=pay=pay
!nan
=pay
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=pay
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!kpj2
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=esk2=esk2
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=esk4
!lcv3
!lcv2
!jut4
!rot1
!byl1
=esk4
=csi2
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=be1
!KOV4
!fth1
!rot3
=esk4 =esk2=esk4
=esk4
=esk4
=esk4
=esk4
=esk2
=esk2
=esk2
=esk2
=esk4
=esk2
=esk4
=esk2
=esk4
=esk4
=esk2
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!lcv3!byl2
=csi4
=csi4 =csi4
=csi4
=csi3
=csi4=csi4
=csi4
=csi4
=csi4
=csi4
!lcv1
!jut1
!byl1
!jut3
=csi2
!jut3
!jut3
!lcv1!jut3
!jut1
!lcv2
!KOV4
=csi2=csi4
=csi3
=csi3=csi3
=csi3
!jut3
!rot3
!jut3
!jut1
!lcv2
!lcv1!jut1
!lcv3
!byl2
!jut4!jut4
!lcv1!lcv1
=csi4
=csi4
=csi1
=csi4
=csi4
=csi4
=csi2
!KOV4!KOV4
!KOV4
!KOV4
!KOV4
=wa4
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=esk4
=esk4
=esk4
=esk2=esk4
=esk4
=csi2
=esk2=csi2 =csi2
=esk4=csi2
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=esk4
=esk2 =esk2
=esk4 =esk4 =esk2=esk4 =esk4
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=esk1
=esk3
=esk4 =esk2=esk4
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=esk4=esk2
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=esk4=esk4=esk2
=esk4
=esk4
=esk4
=esk4
=be7
=ce1
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=ni2
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=esk4
=ble
=ble
=ble=ble
=ble
=ble=ble
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=ble
=ble
=ble
=ble=ble
=ble
!inn3=ble=ble
=ble
=ble
=be3
!rot3
!roy1
!byl1
!byl1
!byl1
=ble
!byl1
=ble
=ble
!pin2
=ble
=irs
!pin1=ble
!pin3!byl1
!inn3
!pin3
!pin2
!pin1
!ale2
!ale2
!ale1
=esk4=esk4
=esk4
=esk4
=esk4
=esk4
=esk3
=esk4
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!ale1
=esk3=esk4
!cot4
=esk4
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=csi1
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=csi4=csi2
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=csi2
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=csi3
=csi2
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=csi1
=csi4
=csi2=csi4
=csi2
!lcv2
=esk4
=esk4
=esk4
!lcv2
!lcv2
!lcv1
!lcv1
=NAR2
=NAR5
=NAR2
=NAR5
=NAR2
=NAR2
=NAR2
=csi1
=csi3
=csi3
=csi2
=csi3
=NAR2
=NAR1
=NAR4
=NAR3
=NAR3
=csi1
=csi4
=csi2=csi1
=csi1 =csi4
=esk4
=csi2
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=esk4
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=esk4
=esk2 =esk2
=esk2
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=sp1
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=ni
!KOV8
=ni
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!lcv2
!mez1
!rot3
!mez1
!lcv1
!rot3
=csi2
!roy1
!roy1
!rot1!mez1
!rot2 !rot1
!lcv1
!roy1
!byl2!byl2!pin1 !roy1
!pin2
!lcv1!rot2
!roy1
!roy1
!rot1
=csi2
!mez1
!rot1
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!ale1
!lcv1
=esk4
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=esk4 =esk4
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=esk2
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!lcv1
!lcv1
!kpj2!ale1
=esk2
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!lcv1
!lcv1
!lcv1
!lcv3
=csi2
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=csi1 =esk2
!KOV1
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=esk4 =esk4
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=esk4
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=esk2
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=esk4
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!lcv3
!lcv1
!lcv2
!cot4
=NAR2
=NAR2
=NAR2
=NAR4
=NAR2
=NAR2
=NAR2
=NAR2
=esk2
=esk2
!lcv2
!cot4
!lcv2
!KOV5=esk4
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!kpj2!lcv1
!lcv1!cot3
!lrd1
=esk4
!lrd1
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!fth1
!fth1
!lrd1
=esk3=esk4
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=esk4 =esk4
!lrd1
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!fth1
!lrd2
!lrd1
!lrd1
!arn2
!lrd1
=esk4
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!lrd1
!lrd1
!lrd1
=esk4 =esk2=esk2
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!lcv2
!lrd1
!lrd1
!lrd1
!qim1
!kpj2
!rot1
!pin2
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!rot3
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!lep
!lep
=NAR4
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!lrd2
!lrd1
!lcv2
!kpj2
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!kpj2
!kpj2
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!lcv2
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!KOV9
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!KOV8
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!lep
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!lsd
!lsd
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!roy1
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!pin3!mez1
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!lcv2
!kpj2
!kpj2
!kpj2
!kpj2
!pin1
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!KOV4
!KOV4
!KOV4
!KOV8
!KOV4
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!roy1!rot3
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!lcv1
!lcv1
!lcv1
!lcv1
!lcv1
!kpj2
!kpj2!kpj2
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!kpj2
!kpj2
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!KOV8
!KOV2
!KOV2
!fth1
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!KOV3
!KOV8
!KOV4
!KOV2
!KOV3
!KOV3
!KOV9
!KOV2
!KOV2 !KOV2
=NAR2
=NAR2
!arn2
!arn2
!arn2
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!arn2
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!lcv2
!lrd2
!kpj2
=NAR2
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=NAR4 =NAR4
!arn2
=NAR2
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=esk4
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!byl1
!byl1
!byl1
!byl1
=esk4
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=NAR4
=esk2=esk4
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!KOV9
!KOV2 !KOV3
!KOV2
=NAR1
!KOV5
!lcv2
=esk2
!lcv1
=NAR4
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=NAR2
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!KOV2
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=NAR2 =NAR2
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=NAR3
=NAR3 =NAR3
=NAR2
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!kpj2
!lcv1
!lcv1
!kpj2
=NAR4
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!KOV6
=NAR4=NAR1
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=NAR4
!kpj2
!lrd1
!kpj2
!lrd2
!cmm4
!qim1
=esk2
!KOV7
!KOV7
!KOV7
!KOV7
!KOV7
!KOV9!KOV8
!KOV5
!KOV8!KOV7
!KOV8
!KOV4
!KOV2
!KOV4
=pay
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!KOV5
!KOV5
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=pay
=pay
=pay
!kpj2
!cmm4
!lrd2
=NAR2
!KOV5
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!KOV9
!KOV5
!mez1
!rot3!rot1
!rot2
=NAR1
!KOV2
!KOV5
!KOV7
=NAR6
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!KOV7
!KOV7
!KOV9
!KOV9
!KOV9
=su
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!rot1
=be1
!KOV9
!KOV5
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!cmm4
!lcv2
!KOV2
!KOV3
!KOV8
!KOV2!KOV2
!KOV2
!KOV9
!KOV4
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!fth1
!KOV5
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!KOV3
!KOV9
!KOV2
!KOV9
=esk3
!lrd2
=NAR1
=NAR4
!KOV2
!KOV2
!KOV9
!KOV2
!KOV2!KOV3
!KOV2!KOV2
!KOV8
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!KOV9
!KOV9
=pay
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=NAR1
=wa4
!fth1
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!KOV9!KOV2
!KOV7!KOV5
!KOV5
!KOV8
!KOV5
!KOV8
!KOV7
!KOV7
!KOV9!KOV7
=csi1
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!fth1
!kpj2
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!kpj2
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!lrd1
=pay
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!lrd1
=pay
!lrd2
!lrd1
!kpj2
!KOV2
!KOV8
!KOV9
!KOV4
!KOV4
!arn2!lrd2
!lrd2
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!KOV2
!KOV8
!KOV9
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!KOV4
!KOV4
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!jut4a
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!lcv1a
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!KOV10
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=le
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!lrd1
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=pa4=pa2 =pa5
=wa6
=pa2=ch1
=pa5=pa4
=pa1=pa7=pa1
=pa3
=pa2
=pa6=pa2
=pa1=pa3
=ch5
=ch4
=ch2
=ch1=ce4
=ch2=ce4
=ce1 =be2
=nu1
=be8
=ce4
=wa4
=be5=ce1
=ce2=ce4
=be2=be4
=be4
=be1
=be8
=be2
=be5 =be5=be4
=be2
=be5=be5
=be4
=be2
=ch2
=ch1
=ch1=ch4
=ch3
=ch4
=ch1
=ch4
=ch2
=ch4
=ch2
=ch2
!qim1
!qim1=ch2
=be6=be2
=ni4
=be3
=be3
=ch1
=ch3=ch1
=be3
=be3
=ni3
=be1=be3
=ni2
=be3=be5
=be3=be3
=be5=be3
=be3=ni2
=be3=be3
=ku3
=ni1 =ku3
=ni3
=ku3
=be3
=ni1=ni5
=ni1
=ku4
=ku1
=ni5
=ku2
=ku3=ku1
=ch4
=ch1 =ch3=ch1
=ch4=ch2=ch4=ch1
=ch3=ch4
=ch4
=ch4=ch2
=ch1=ch1
=ch4
=ch4=ch4
=ch4
=ch3=ch2 =ch1
=ch1
=ch4=ch1 =ch2
=ch1
=ch3=ch2
=ch2=ch2
=ch4
!lep
=ce1
=ch2
=be1
=be1
=be6=ch1=ch2=ch2
=ch1=ch4
=ch2
=ch3
=be3=ch3=ch3
=ch1
=ch4
=ch1
=ch4
=be6=be3
=sp2
=sp2
=sp1
=pa1
=pa5
=pa3
=be5
=pa2
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=ch2
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=sp1
=ni1
=be3
=be3
=be3
=ku3
=wa2
=wa3
=sp2
=sp1
=wa2
=nu1
=ch2
=nu1=nu1
=ce2
=be1
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=ch2
=pa3
=ce4
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=pa1=pa1
=ch2
=nu1
=nu1
=ch1=ch2
=ni4
=ni4=ni4
=ch2
=ni6
=ni4
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=ni1
=be5
=ni1
=ni4
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=ni6
=ni4
=ni1
=ni4
=ni6
=ni6
=pa1
=ni6
=kk
=ce1
=nu1
=ch1
=ce3
=ce3
=nu1
=ni1
=pa1 =pa6
=pa7
=pa1 =pa6
=pa1=ch1
=ch2
=ch1
=ch2
=ni4
=ni1
=ni6 =ni1
=ni1
=ch2
=ni4
=ni4
=ni4=ni1=ni1
=ni4
=ni1
=ni1
=ni1
=ni6
=ni1
=ch4=ch4
=ch4
=be1
=be1
=ce1=ce2
=be2 =be4
=ce1
=ce3
=ni1
=be1
=ni4
=be2
=ni4
=ni4
=ni2 =ni4
=ch1
=ch3
=ni1
=ch3
=ni1
=ch1
=ch2
=ni1
=ce4
=ce2=ce4
=ce2 =be3
=be3
=be1
=be1
=be1
=be2
=be2
=be1
=be1
=be8
=be2
=be2=be3=be5
=be3
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=be2
=be3
=be3
=be3
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=ni2
=ni1
=ni2=ni4
=ni2=ni1
=ni2
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=be5
=pa7
=pa4
=ni
=ni6
=be1
=be1
=ch3
=nu1=ch3
=nu1
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=ni4
=ni4
=ch4
=pa1
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=kk
=ni6=ni1
=ni1
=ni4=ni4
=ni4
=ni2
=ni2
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=be1=be1
=be1
=be1
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=be1
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=wa2
=ni1
=ni1
=kk
=ni6 =kk
=be1
=be1
=pa7
=pa1
=pa6
=wa2
=wa4 =wa2
=ch1
=ch3
=be2
=ni6
=wa4
=ni1
=ni1=wa5 =ni1
=wa4
=wa4
=ni1
=wa3
=wa2
=wa4
=ni2
=sp1
=wa5
=ch4
=wa2
=wa5
=wa2
=nu1
=su
=NAR1
=NAR4
=NAR1
=su
=NAR4
=NAR1
=NAR1
!KOV9
!KOV4!KOV4
!KOV4
!KOV5
=NAR1
!KOV5
=NAR1
=NAR1
=NAR2
=NAR1
=NAR4
=NAR2
=NAR1
=NAR1
=NAR2
!KOV4
!KOV4
=wa3
=NAR1=wa2
=wa4
=wa4
=ch4
!KOV9
!KOV9
")
")
")
")
Détroit d'Hudson
Baie d'Hudson
HavrePecten
Lac Leclair
Rivière
Korak
Rivière Kuu vvaluk
Lac Chukotat
Lac Nituk
Lac Bélanger
LacParent
LacSpartan
LacEsker
NuvilicLacs
LacCécilia
Lac Beauparlant
ÎleNatirnaalik
Vallée Narsajuaq
Lac Nantais
LacAllemand
Rivière d
e
Povungnituk
LacBylot
LacJuet
LacLanyan
Lac Rouxel
LacVergons
Lac Nallusarqituq
LacVanasse
LacBilson
Lac Péloquin
LacLaflamme
LacSaint-Germain
LacBelleau
LacKapijuq
Lac Tasiujaaluk
Lac Fargues
Lac Ivitaaqqut
LacQalluujaup
Lac Rocbrune
LacQamaniq
LacTalluup
LacQanartaliup Tasinga
LacVigneau
Rivière Chukotat
Lac Tasialuk
Lac Amarurtuup
Rivière Kovik
Lac Françoys - Malherbe
Lac Wat ts
Lac Grunérite
Juet
Laïla
Anore
Goshawk
Peltier
Roy No 2
Roy No 3
Roy No 1
Gerfaut-1
Lac Parent
Goshawk Ouest
Lac Spartan (Zone No 70)
Zel
Plug
Lima
Kilo
IndiaAlpha
Tripod
Tootoo
Orchan
Echo-2
Area 4
Echo-1Echo-3
Inuluk
Cecilia
Charlie
Lac Weir
Allemand
Zone B-4
Zone B-5
Cible 12
Lac Kapaa
Expo-East
Lac Hubert
Swarm Hill
Beta-Getty
Delta WestDelta East
Dan's Zone
Ladyfinger
Lac Gossan
Riv. Kovik
ÉCH. 124822
Juliet East
Goshawk Sud
Ekwan River
ÉCH. 124630
ÉCH. 124767
Expo Ungava
Éch. #198418
Éch. #198839
Éch. #198412
Éch. #198434
Lac Gossan-2
Lac Vaillant
Mesamax West
Lataille Sud
Lac Chukotat
Indice No 19
Frontier East
Tazin No X-11
Asarco No X-1Lac Gossan-SE
Rinfret North
Tazin No X-21
Lataille Nord
Lac Grunérite
Frontier South
Chukotat Ouest
Little Pov - 1
Deep Mag Model
Little Pov - 2
Lac Chasse-Est
Lac Lessard-SE
Lac Fargues-SE
Murray (Zone A)
Lac Chukotat-SO
Deception Ridges
Frontier Central
Delta (Zone D-8)
Indice Churchill
Bravo (Zone B-8)
Raglan (Katinniq)
Delta (Zone Nord)
Pointe du Profond
Ranlux (Zone No 9)
Raglan (Zones 5-8)
Raglan (Zone No 2)
Raglan (Zone No 3)
Hudson (Zone No 1)
Hudson (Zone No 6)
Lac Ekwan (Zone B)Lac Ekwan (Zone A)
Raglan (Donaldson)
Christine A. Petch
Lac Ekwan (Zone C)
Raglan (Lac Cross)
Cominga (Zone No 1)
Deception Ridge-Est
Ron Roy (Groupe No)
Baie Kettlestone-NE
Cominga (Zone No 16)
Hudson (Zone No 4-A)
Cominga (Zone No 14)
Cominga (Zone No 17)
Cominga (Zone No 18)
Ron Roy (Groupe No 1)
Indice Getty (Zone A)
Ron Roy (Groupe No 3)
Delta (Zones D-1 à D-6)
Mont de Povungnituk-Nord
Raglan (Zones C-2 et C-1)
Cominga (Zones Nos 4 et 5)
Raglan (Zones Nos 13 et 14)
Petite Rivière de Povungnituk
Raglan (Zone No 9 du Lac East)
Hasik, Maeckelburg & Giovanezzo
Raglan (Zone South Sill du Lac East)
Raglan (Boundary West, Zones 9 et 12)
Cominga (Zones Nos 8, 9, 10, 11 et 12)
Raglan (Boundary East, Zones 10 et 11)
Raglan (West Boundary, Zones 15 et 16)
Delta (Zone D-9)
Bravo (Zone B-7)
Zones B1, B2 et B3
Delta Nord (Extension Est)
Cominga (Zones 2, 3, 6 et 7)
35I04
35I0235I03
35I0535I06
35J0335J04 35J0135J02
35J06 35J0835J0735J05
35F0135F02
35F0335F04
35F0835F07
35F0535F06
35L01
35F1035F09
35B14
35F11
35B1535A13
35B13
35F12
35B16
35A1635A15
35L08
35A14
25E04
35F13
35F1535F14
35F16
25E05
35C1435C15
35C1335D16 25D13
35C16
35E09 25E12
35H04
35H0235H01
35E16
35H03
35H07
35H05
35H08
35K0235K03
35K04
35K01
35H06
35H12
35H0935H10
35K08
35K05
35K0735K06
35H11
35G04 35G03 35G0135G02
35H13
35H1635H15
35H14
35G06 35G0835G05 35G07
35G10 35G0935G1135G12
35G1535G13 35G1635G14
=
Salluit
Ivujivik
Akulivik
Kangiqsujuaq
71°30'0"W
71°30'0"W
72°0'0"W
72°0'0"W
72°30'0"W
72°30'0"W
73°0'0"W
73°0'0"W
73°30'0"W
73°30'0"W
74°0'0"W
74°0'0"W
74°30'0"W
74°30'0"W
75°0'0"W
75°0'0"W
75°30'0"W
75°30'0"W
76°0'0"W
76°0'0"W
76°30'0"W
76°30'0"W
77°0'0"W
77°0'0"W
77°30'0"W
77°30'0"W
78°0'0"W
78°0'0"W
62°30'0"N
62°30'0"N
62°15'0"N
62°15'0"N
62°0'0"N
62°0'0"N
61°45'0"N
61°45'0"N
61°30'0"N
61°30'0"N
61°15'0"N
61°15'0"N
61°0'0"N
61°0'0"N
60°45'0"N
60°45'0"N
LÉGENDE STRATIGRAPHIQUE
OROGÈNE DE L'UNGAVA
NÉOPROTÉROZOÏQUE
E s s a im d e Fr a n k l i n
D i abase
PALÉOP ROTÉROZOÏQUE
ARC DE N ARS AJU AQ
S u i te ta r d i ve (env . 1 ,8 0 - 1 , 7 4 G a )
Monzog r an i t e à b i o t i t e
S yénog ran i t e
S u i te p l u t o n i qu e r éc e n t e (env . 1 , 8 4 - 1 , 82 Ga )
Monzog r an i t e + s yénog r an i t e avec b i o t i t e ± ho r nb l ende ; monzod i o r i t eà c l i n opyr o xène ± ho rnb l e nde ± b i o t i t e
Tona l i t e + g r anod io r i t e à ho r nb l e nde + b i o t i t e ; v e i n es de monzog r an i t eà b i o t i t e
D i o r i t e qua r t z i t i que à ho r nb l ende ± b i o t i t e ; d i o r i t e + monzod i o r i t e àho r nb l ende + b i o t i t e ; p y r o xén i t e à c l i n opyr o xène + ho r nb l ende + b i o t i t e ;ve i n e s de monzog ran i t e à b i o t i t e
S u i te p l u t o n i qu e a nc i e n ne (env . 1 , 86 - 1 ,8 5 G a )
Gne i s s avec t ona l i t e à b i o t i t e ± ho r nb l ende e t d i o r i t e qua r t z i q ue àho r nb l e nde ± b i o t i t e s t r a t i f i é e s ; g r anod io r i t e à b i o t i t e ; v e i n es demonzog r an i t e à b i o t i t e
Gr o u pe d e S u g l u k
Sem i - pé l i t e , q ua r t z i t e , r oche séd imen t a i r e f e r r u g i n euse , pé l i t e , marb r e , ro checa l c o -s i l i c a t ée , amph i bo l i t e
DOM AINE NORD
S u i te d e C ap e S m i t h (env . 1 , 9 0 - 1 , 84 G a )
Granod i o r i t e , g ran i t e , t o na l i t e à amph i bo l e + b io t i t e , a l a sk i t e
D i o r i t e , d i o r i t e qua r t z i f è r e , monzon i t e , monzon i t e qua r t z i f è r e , t o na l i t e
Gabb r o à g r a i n mo yen , mésoc r a t e à mé l anoc r a te
Pé r i d o t i t e , p yr o xén i t e
Gr o u pe d e S p ar t a n
Vo l c anoc l as t i t e s
S i l t s t o ne , ph y l l a des , g r ès l oc a l emen t c ong l omé ra t i q ue
G r o u pe d e P ar e n t (env . 1 , 9 2 - 1 ,8 6 G a )
Sch i s t e à p l a g i o c l as e + sé r i c i t e + ank é r i t e
S i l t s t o ne , g r è s , s c h i s t e à qua r t z + f e l ds pa t h + b io t i t e
Rh yo l i t e , s ch i s te à f e l ds pa t h + b i o t i t e + amph i bo l e
Basa l t e à pyr o xène
Basa l t e à p l ag i o c l a se
Basa l t e aphan i t i q ue
Tu f à b l o cs
Tu f à g ra i n f i n , à l a p i l l i s e t / o u à c r i s t a u x , t u f r ubané
Gr o u pe d e W a t t s (env . 2 , 0 0 Ga )
Basa l t e
D i abase , d yk es en feu i l l e t s
Gabb r o l i t é
P yr o xén i t e
Pé r i d o t i t e
Dun i t e
DOM AINE SUD
P l u to n d e P e c t e n H ar b o ur
Granod i o r i t e , t o na l i t e à amph i bo l e + b i o t i t e
S u i te d u l ac E s k er (env . 1 , 8 9 - 1 , 8 7 G a)
Pé r i d o t i t e à enc l aves r ougeâ tr es de gabb ro à c l i n opyro xèn e ± o r t h opyr o xène
Gabb ro
P yr o xén i t e
Pé r i d o t i t e
Dun i t e
S u i te d u l ac B é l an g er (env . 2 , 0 4 - 1 , 9 6 G a )
D i abase , m i c r ogabb ro
Gr o u pe d e C h uk o t a t (env . 1 , 8 9 - 1 , 87 Ga )
Mud ro ck , vo l c anoc l a s t i t e
Basa l t e à p l ag i o c l a se
Basa l t e à pyr o xène + p l ag i oc l as e
Basa l t e à pyr o xène
Basa l t e à o l i v i n e
Gr o u pe d e P o vu n g n i t u k
F or m a t i o n de N u v i l i c
Ca l c a i r e , c a l c a i re do l om i t i q ue
Grès , s i l t s t o ne
F or m a t i o n de C é c i l i a (env . 1 ,9 6 G a )
S i l t s t o ne , g r è s e t cong l oméra t ; ca l c a i r e , c a l c a i r e do l om i t i que ; c he r t ,
p h y l l a des
Rh yo l i t e , l av e f e l s i que
Basa l t e a l c a l i n , b asan i t e , p hono l i t e e t t r ac h y t e
Vo l c anoc l as t i t e s
F or m a t i o n de B e a u p ar l a n t (env . 2 , 0 4 - 1 , 96 Ga )
Ca l c a i r e do l om i t i que
Grès a rk o s i que
Fo rma t i o n de f e r s i l i c a t é e e t ca r bona tée
Vo l c anoc l as t i t e s
Rh yo l i t e e t l av e f e l s i q ue
Ph y l l a des
S i l t s t o ne , g r è s e t cong l oméra t
Basa l t e , amph ibo l i t e
F or m a t i o n de N a t i r na a l i k
Do lom ie , ph y l l a des
F or m a t i o n de N i t u k (> 2 ,0 4 M a )
Qua r t z i t e , s c h i s t e à qua r t z + f e l dspa t h + b i o t i t e ± mus cov i t e ± g r ena t± amph i bo l e
Grè s m ic acé
Fo rma t i o n de f e r
Basa l t e
Ca l c a i r e , c a l c a i re do l om i t i q ue
Ph y l l a des
S i l t s t o ne , g r è s e t cong l oméra t
F or m a t i o n d u l ac L ec l a i r
Tu f à l a p i l l i s e t l a ve ca r bona t i t i que
F or m a t i o n de K u u v va l u k
Sch i s t e à qua r t z + ac t i n o t e + b i o t i t e
Fo rma t i o n de f e r
Sch i s t e à g r uné r i t e + magné t i t e
Qua r t z i t e à magné t i t e
F or m a t i o n de K o r a k
Grès a rko s i que , c ong l omé ra t
ARCHÉEN
ANTIFORM E DE KOVIK (env. 3,22 - 2 ,74 Ga)
Syénog ran i t e à b i o t i t e ± ho r nb l e nde ; pegma t i t e g ran i t i q ue
Monzog r an i t e e t monzon i t e po r ph yr i que à b i o t i t e ± ho r nb l ende ±ép i do t e± t i t a n i t e
Granod i o r i t e e t t o na l i t e à b i o t i t e ± ho r nb l e nde ± ép ido t e ± t i t an i t e( l oc a l emen t avec enc l a ve s de r o ches ma f i ques )
Tona l i t e e t g r anod io r i t e à ho r nb l ende + b io t i t e ; v e i n es de monzog r an i t eà b i o t i t e
Tona l i t e e t d i o r i t e qua r t z i t i q ue à ho rnb l ende + b i o t i t e ; v e i n es demonzog r an i t e à b i o t i t e
Tona l i t e e t g r anod io r i t e à b i o t i t e ± ho r nb l e nde ± ép ido t e ± t i t an i t e ± a l l an i t e( en c l aves de r oches ma f i q ues r a r es ) ; v e i n e s de monzog ran i t e à b i o t i t e ;g ne i s s to na l i t i q ue , gne i s s g ranod i o r i t i q ue
Tona l i t e e t g r anod io r i t e à b i o t i t e ± ho r nb l e nde ± ép ido t e ± t i t an i t e ± a l l an i t e( en c l ave s de r oches ma f i q ues abondan te s ) ; v e i n es de monzog r an i t e à b i o t i t e
A l eu r i t e , p é l i t e , ps amm i t e , qua r t z i t e , c ong l omé ra t ; ma rb r e ; amph ibo l i t e ;
p a r agne i s s à b i o t i t e ± g rena t ± co r d i é r i t e ± s i l l im an i t e ; v e i n es demonzog r an i t e à b i o t i t e
D i o r i t e qua r t z i que à ho r nb l ende ± b i o t i t e ± magné t i t e ± c l i n opyr o xène ;gabb r o , gabb ro ano r th o s i t i que ; amph ibo l i t e à ho r nb l ende + b i o t i t e ;p é r i d o t i t e , p y r o xén i t e ; v e i n e s de monzog r an i t e à b i o t i t e
Amph i bo l i t e ; b a sa l t e ; t u f à l a p i l l is e t à c r i s t au x
PROVINCE DU SUPÉRIEUR*
PROTÉROZOÏQUE
D yk e s d e P o i n t e R a u d o t ( ~ 2 0 00 M a)
Dyk es de d i abase e t de gabb r o , homogènes , mas s i f s , t e x t u r e oph i t i que , g r a i n f i nà g r os s i e r ; s u r f ac e f r a î c he g r i s b l e u t é , p a t i n e b r un ve r dâ t r e à b r un no i r â t r e ;p os sèden t une o r i e n ta t i o n géné r a l e NE-SW
D yk e s d e l a r i v i è r e I r s ua q
Dyk es de d i abase , homogènes , mass i f s , t e x t u re oph i t i q ue , g ra i n moyen àg ro ss i e r ; r oc he ve r t f o ncé ; po ssèden t l o c a l emen t un c l i v age e t uneo r i en t a t i o n géné ra l e N-S à NNE-SSW
D yk e s d e l a R i v i è r e P a yn e (> 2 00 0 M a p ar d a t a t i o n K / A r , F a hr i g e t a l . , 19 8 5 )
Dyk es de d i abase e t de gabb r o , homogènes , mas s i f s , magné t i q ue , t e x t u r eoph i t i q ue , g r a i n f i n à aphan i t i q ue , s u r f ace f r a î c he g r i s b l eu té , p a t i ne b r unve r dâ t r e à b r un no i r â t r e ; po ssèden t une o r i en t a t i o n géné ra l e NW -SE
D yk e s d e K l o t z (~ 2 2 09 M a p a r da t a t i o n U /P b , B u c h a n e t a l . , 1 9 98 )
Dyk es de d i abase e t de gabb r o , homogènes , mass i f s , t e x t u r e oph i t i que , g r a i nmoyen à g r os s i e r ; r o che ve r t moyen ; po ssèden t une o r i e n t a t i on géné r a l e ESE-WNW à E-W
D i a t r è m e s de K u u v va l u k
Lamp roph yr e u l t r ama f i q ue b r é ch i que
ARCHÉEN
C o m pl e xe d e L e R o y
D i a t e x i t e à b i o t i t e + g r ena t ( n on subd i v i sée ) : à b i o t i t e + g r ena t ± co r d i é r i t e ±s i l l iman i t e ; c on t i en t e n t r e 25 e t 80 % de l eucosome f e l s i que àpo r phyr ob l as t es de g r ena t ± o r t h opyr o xène ; p r o t o l i t h e hé té r ogène ,l e ucoc r a te à mésoc ra t e e t à g r a i n g ro ss i e r (p s amm i t e ) ou homogène ,mé l anoc ra t e e t à g r a i n f i n (mé t apé l i t e ) ; c on t i e n t des n i v eaux de f o rma t i o nde fe r ; r oc he b r un r ou i l l e l eu cosome d 'âge de c r i s t a l l i s a t i on de 2668 ± 22Mapa r da t a t i o n U /Pb su r z i r c on
S u i te d e C o ut ur e
Pyro xén i t e mass i v e
D i o r i t e à o r t hop yr o xène
C e i n tu r e d e J u e t
Roches mé ta vo l c an i q ues ma f i q ues : ba sa l t e c ous s i né f o r t emen t t r an sposé ,amph ibo l i t e à ac t i n o t e ± ho rnb le nde , g r a i n f i n à mo yen , mass i v es à f o l i ée s ,ve r t f o n cé
Gabb r o : à ho r nb l ende , mésoc r a t e , homogène , g r a i n f i n à moyen ,mass i f à f o l i é , t e x tu r e suboph i t i q ue l o ca l emen t p ré s e r v ée
Roches vo l c anoc l a s t i q ue s i n d i f f é ren c i é es : s ch i s t e à sé r i c i t e , tu fa phan i t i q ue , à c r i s t a u x e t à l a p i l l i s (mo i ns de 3 cm ) , c ompos i t i o n ma f i q ue àfe l s i q ue , l oc a l emen t l am i nées
Roches séd imen t a i re s e t mé ta séd imen t a i r e s : qua r t z i t e , s i l t s t o ne , g r ès ,cong l oméra t monogén i que e t po l ygén i que , pa r agne i ss à b i o t i t e ± g r ena t± c o r d i é r i t e ± s i l l im an i t e e t f o rma t i o n de f e r ; l i t age p r ima i r e l oc a l emen t b i e np ré s e r v é
C e i n tu r e d e A l l e m a n d
Sch i s t e à muscov i t e
Mé t abasa l t e
S u i te d e M a cM a h o n
Tona l i t e m i gma t i t i q ue , f o l i é e ou gne i s s i q ue , à o r t hop yr o xène , c l i n op yr o xène ,ho r nb l e nde e t b i o t i t e ; l a t o na l i t e es t i n t e r c a l é e avec des phases d i o r i t i que s ,t r o ndh j ém i t i q ues e t g r anod i o r i t i que s ; l es ro c hes de l ' u n i t é c on t i e nnen t en t r e20 e t 70 % de mob i l i s a t g r an i t i q ue sous f o rme de ve i n es pa r a l l è l e s à l afo l i a t i o n e t i n j ec té e s « l i t p a r l i t »
S u i te d e L e p e l l e
Granod i o r i t e , mas s i ve ou fo l i é e , l oc a l emen t po r phyr o ïde , à b i o t i t e ,c l i n op yr o xène , magné t i t e ± o r t h opyr o xène ± ho rnb l e nde ; l a g ranod i o r i t e e s ti n te r ca l ée avec des phases g r an i t i q ues e t monzog r an i t ique s ; l ' un i t é c on t i e n ten t r e <1 e t 15 % d ' enc l a ves de r oc hes ma f i q ues (d i o r i t e , amph i bo l i t e ) e t depa r agne i s s ; l ' u n i t é i n c l u t d es ve i n e s e t des d yk es de g r an i t e pegma t i t i q ue qu ii n t r u den t l a l i t h o l o g i e p r i nc i pa l e
S u i te d e L e s d i g u iè r e s
Tona l i t e m igma t i t i q ue à ho rnb l ende e t b i o t i t e
S u i te d e L er i d o n
Gran i t e po rph yr o ïd e à b i o t i t e , magné t i t e ± ho r nb l e nde , mass i f ou l égè r emen tfo l i é , l oc a l emen t pegma t i t i q ue ; l ' un i t é i nc l u t d es ve i ne s e t des dykes decompos i t i o n g r an i t i que qu i i n t r uden t l a l i th o l o g i e p r i n c i p a l e
Granod i o r i t e e t g r an i t e f o l i é s , à b i o t i t e e t ho rnb l e nde ; l ' u n i t é c on t i e n tl o ca l emen t des phases monzon i t i que s ; l ' u n i t é i n c l u t d es ve i n es e t de s dyk esde compos i t i o n g r an i t i que qu i i n t r uden t l a l i t ho l o g i e p r i nc i p a l e
S u i te d e L a C h e vr o t i è r e
Granod i o r i t e : à b i o t i t e ± ho r nb l e nde , l e u coc ra t e , homogène , mass i ve àfo l i ée , g r a i n mo yen à g ro ss i e r , é qu i g r anu l a i re ; r o che g r i s r ougeâ t r e àb l anchâ t r e , c on t i en t des phases g r an i t i q ues en con t ac t d i f f us
Gran i t e , monzogr an i t e e t monzon i t e qua r t z i f è r e , mass i f s ou f o l i é s ,h omogènes , l o ca l emen t m y l on i t i sé s , à b i o t i t e , magné t i t e ± ho rnb l e nde ;l ' un i t é i nc l u t d es ve i n es e t des dyk es de compos i t i o n g r an i t i q ue qu ii n t r u den t l a l i t h o l o g i e p r i nc i pa l e
Monzog r an i t e , g r anod i o r i t e à monzon i t e qua r t z i f è r e po r ph yr i q ue ( nonsubd i v i s és ) : à b i o t i t e ± ho r nb l ende ± c l i nop yr o xène , homogènes , f o l i és ,p o r ph yr i q ues à mégapo r ph yr i q ues avec des phénoc r i s t a u x de fe l d spa t hpo t as s i q ue a t t e i g nan t 5 cm de l ongueu r ; r oche g r i s r os é à r ougeâ t r e
Gran i t e po rph yr o ïde à c l i n op y r o xène
S u i te d e P i n g u q
Granod i o r i t e : à b i o t i t e ± ho r nb l e nde ± qua r t z b l e u , l e ucoc r a t e , h omogène ,mass i ve à fo l i é e , g r a i n mo yen à g r o ss i e r ; r oc he b l anc ro sé ; c on t i e n t desenc l a ve s de r o che ma f i q ue à u l t r ama f i q ue
Gran i t e : à b i o t i t e ± ho r nb l e nde ± qua r t z b l e u , homogène , mass i f à f o l i é ,g ra i n moyen à g r os s i e r , équ i g r anu l a i r e ; r oc he b l anc ro sé ; c on t i e n t desenc l a ve s de r o che ma f i q ue à u l t r ama f i q ue
Monzog r an i t e , g r anod i o r i t e à monzon i t e qua r tz i f è r e à po r phyr ob l as t es dem ic r o c l i n e ( non subd i v i sés ) : à b i o t i t e ± ho r nb l ende ± c l i n opyr o xène ±qua r t z b l eu , f o l i és à m y l on i t i q ues , c r i s t au x de m ic r oc l i ne po r ph yr ob l a s t i q ueà mégapo r ph yr ob l a s t i q ue a t t e i g nan t 7 cm de l ongueu r ; r o c he g r i s r os é àr ougeâ t r e ( âges de 2727 , 0 ± 2 , 1 Ma e t 2725 , 2 ± 4 , 4 Ma pa r da ta t i o n U /Pb
su r z i r con )
S u i te d e B yl o t
Gran i t e à g r anod i o r i t e à b i o t i t e ± ho rnb l e nde , hé té r ogène , hé t é r og r anu l a i re ,t e x t u r e s ac cha r o ïd a l e , aspec t gne i ss i q ue ; c on t i en t d es enc l ave sd ' amph i bo l i t e , d es r es t i t e s de pa r agne i ss , d es amas e t des sch l i e r en s deb i o t i t e , f o l i a t i o n ondu l an t e , g r i s r os é ; a spec t de d i a t e x i t e
Tona l i t e à t r o ndh j ém i t e à b i o t i t e ± ho r nb l ende , hé té r og r anu l a i r es , t e x t u r esa ccha ro ïda l e , a spec t gne i s s i q ue ; con t i e n t des enc l av es d ' amph ibo l i t e , d esr es t i t e s de pa ragne i ss , d es amas e t de s sch l i e r e ns de b i o t i t e , f o l i a t i onondu l a n te , g r i s moyen ; as pec t de d i a t e x i t e
C o m pl e xe d e Q im u ss i n g u at
Tona l i t e gne i ss i q ue ou f o l i é e à o r t h opyr o xène , c l i nop yr o xène , hor nb l e nde e tb i o t i t e ; l a t o na l i t e es t i n t e r c a l é e avec des phases d i o r i t i q ue s ,t r o ndh j ém i t i q ues , g r anod i o r i t i q ues e t g r an i t i q ues ; l e s r o ches de l ' un i t é s on tm igma t i s ées e t c on t i e nnen t en t r e 10 e t 60 % de mob i l i s a t f e l s i que e t en t r e1 e t 10 % d ' enc l av e s ma f i ques
C o m pl e xe d e M é z ar d
Roche mé t avo l c an i que de compos i t i o n ma f i que : à ho r nb l e nde ± b i o t i t e± c l i n op yr o xène ± o r t hop yr o xène , f o l i é e ou g r anob l a s t i que ; con t i en t < 20 %de l eucosome f e l s i q ue à c l i n op yr o xène ± o r t h opyr o xène ; c on t i e n t l o c a l emen tdes r o ches de compos i t i on f e l s i que e t de s tu f s f e l s i q ues i n t e rd i g i t é s avecdes r o ches mé t a séd imen ta i r e s
C o m pl e xe d ’ I n n u k s ua c
Roches vo l c anoc l a s t i q ue s fe l s i q ues : t u f a phan i t i q ue , à c r i s t a u x e t à l a p i l l i s(mo i ns de 3 cm ) , l o c a l emen t l am i nées , s ch i s t e à sé r i c i t e , c on t i e n t de l aho r nb l e nde
S u i te a l c a l i n e d e K i m ber
Syén i t e à néphé l i n e ; c on t i en t l o ca l emen t de l a b i o t i t e e t de l a s oda l i t e
C o m pl e xe d e N a nt a is
Mé tabasa l t e , g ne i ss ma f i q ue à ho rnb l e nde , p l ag i o c l ase ± g r ena t ± b i o t i t e± c l i n op yr o xène ; l ' u n i t é peu t con ten i r de pe t i t es quan t i t és de mé t a vo l c an i t e si n te rméd i a i r es e t f e l s i ques a i ns i q ue des r o ches u l t rama f i q ues ( v o l c an i t esou f i l o n -c ouches ) f o l i é es
S u i te d e K a p i j u q
Tona l i t e gne i ss i q ue ou f o l i é e , l oc a l emen t m y l on i ti q ue , à b i o t i t e , h o rnb l e nde± c l i n op yr o xène ; l a t o na l i t e e s t i n t e rc a l é e avec des phases d io r i t i q ues ,
t r o ndh j ém i t i q ues , g r anod i o r i t i q ues e t g r an i t i q ues ; l e s r o ches de l ' un i t écon t i ennen t en t r e 5 % e t 30 % de mob i l i sa t f e l s i que e t en t r e 5 % e t 25 %d ' enc l a ves ma f i q ues
S u i te d e R oc h e f or t
Tona l i t e g r an i t i s ée hé té r ogène : à b i o t i t e ± ho r nb l ende , l e ucoc r a t e , f o l i é e àfa i b l emen t f o l i é e , g r a i n f i n à moyen ; c on t i en t des i n j e c t i o n s de g ran i t eho l o l eu coc r a t e e t de s phases g ran i t i q ues en con t a c t di f f us ; r oche g r i s pâ l eà g r i s r os é
Tona l i t e hé t é r ogène : à ho r nb l e nde + b io t i t e ; c on t i e n t d e nombreusesenc l a ve s de gne i ss ma f i q ue e t d ' amph i bo l i t e (a ss im i l a t i on de mé tabasa l t e ) ;comp rend des t ona l i t e s homogènes e t f o l i ée s e t des i n j e c t i o ns g r an i t i que s ;r oche g r i s r os é
Tona l i t e à t r o ndh j ém i t e homogène ( non subd i v i s ée ) : à b i o t i t e ± ho r nb l ende ,l e ucoc r a te à mésoc ra t e , homogène , mass i ve , f o l i é e ou r ubanée , peu tcon ten i r de s enc l a v es de ro ches i n t e rméd i a i r e s à ma f i q ues ( âges dec r i s ta l l i s a t i o n de 2766 ± 2 Ma , 2807 , 2 ± 9 , 2 Ma e t 2829 , 8 ± 4 , 6 Ma pa rda t a t i o n U /Pb su r z i r c on )
S u i te d e F ar i b a u l t - T h ur y
Tona l i t e gne i ss i que ou f o l i é e à ho rnb l ende e t b i o t i t e ; l a t ona l i t e e s ti n te r ca l ée avec des phases d i o r i t i q ues , t r ondh j ém i t i q ues , g r anod i o r i t i ques e tg ran i t i q ues ; l e s r oches de l ' u n i t é con t i ennen t en t re 5 e t 50 % de mob i l i s a tf e l s i q ue e t en t r e 5 e t 25 % d ' enc l a ves ma f i ques
Tona l i t e gne i ss i que à enc l a ves maf i ques : l ' un i t é c on t i e n t , dans demo i nd r e s p ropo r t i o n s , des phases d i o r i t i ques , t r ondh j ém i t i q ues ,g ranod i o r i t i q ues e t g r an i t i q ues ; l ' u n i t é con t i e n t en t r e 5 % e t 50 % demob i l i s a t f e l s i q ue e t > 25 % d 'enc l aves maf i q ues
C o m pl e xe d ’ Ar n a u d
Mé tabasa l t e , gne i ss ma f i que à ho rnb l ende , p l ag i o c l ase ± g r ena t ± b i o t i t e± c l i n op yr o xène ; des re l i q ues de te x t u r es vo l c an i ques (c ou l ée couss i née ,b rè che de cou l ée ) son t l o ca l emen t p r ése rv ées ; l ' u n i t é peu t con ten i r depe t i t es quan t i t é s d ' u l t rama f i t e ( v o l c an i t es ou f i l on s -c ouches ) , depa r agne i s s , de marb r e e t de f o rma t i o n de f e r
LÉGENDE LITHOLOGIQUE
NÉOPROTÉROZOÏQUE
Dyk e de d i abase
Gîtes aurifères
Gîtes de métaux usuels
Éléments linéaires
Faille de nature indéterminée
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Faille de chevauchement inverse
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Faille d'effondrement
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�Faille de décrochement dextre
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�Faille de décrochement senestre
Contact géologique
Mine active
Gisement avec tonnage évalué
Gîte travaillé
Indice
Gîte travaillé
Indice
Métadonnées
Système de référence géodésique NAD 83
Projection cartographique Conforme conique de Lambert
Longitude d'origine (méridien central) 75° ouest
Latitude d'origine (équateur) 44° nord
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le=
ku1=
ku2=
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KOV10!
KOV9!
KOV8!
KOV7!
KOV6!
KOV5!
KOV4!
KOV3!
KOV2!
KOV1!
ni2=
ni3=
ni4=
ni5=
ni6=
ni=
na=
be1=
be2=
be3=
be4=
be5=
be6=
be7=
be8=
ce1=
ce2=
ce3=
ce4=
nu1=
nu2=
ch1=
ch5=
ch4=
ch3=
ch2=
fra2
NAR4=
NAR3=
NAR2=
NAR6=
NAR5=
su=
NAR1=
csi4=
csi3=
csi2=
csi1=
sp2=
pa3=
pa4=
pa5=
pa6=
pa7=
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sp1=
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pa1=
wa6=
wa5=
wa4=
wa3=
wa2=
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pec =
esk5=
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ble =
I3B
pra?
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pay=
roy1!
kuv?
ktz=
jut3!
jut4a!
jut4!
cot3!
cot4!
cmm4!
ale1!
ale2!
jut1!
lrd1!
lrd2!
lsd!
lep!
lcv3!
lcv2!
lcv1!
lcv1a!
pin3!
pin2!
pin1!
byl2!
byl1!
qim1!
mez1!
inn3!
kmb!
nan!
kpj2!
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Sources
Données Organisme Année
Réalisation
Compilation et interprétation géologique : D. Lamothe (2007), M. Simard (2006)
Assistance technique : Frédéric St-Pierre
Production : Ministère des Ressources naturelles et de la Faune, Géologie Québec
DV 2007-03 C001
d'Hudson
Détroit
Baied'Hudson
Baied'Ungava
de
Puvirnituq
Rivièr
e
Feuilles
aux
Rivière
Kok
soak
Rivière
Aupaluk
Quaqtaq
Salluit
Tasiujaq
Ivujivik
Akulivik
Inukjuak
KangirsukPuvirnituq
Kangiqsujuaq
Kuujjuaq
80°W
76°W
76°W
72°W
72°W 68°W
68°W
58°N
58°N
60°N
60°N
62°N
62°N
Unités tectonostratigraphiques
Arc de Narsajuaq
Antiforme de Kovik
Domaine Nord
Domaine Sud
Province du Supérieur
1/ 3 000 000
0 25 50 75 km
Compilation géologique de l'Orogène de l'Ungava
Cette carte est extraite de la publication suivante :
Lamothe, D., 2007 - Lexique stratigraphique de l’Orogène de l’Ungava. Ministère des Ressources naturelles et de la Faune, Québec; DV 2007-03, 61 pages, 1 carte.
1 / 250 000
0 10 205 km
LacPingualuk
BaieKovik
Cap Wolstenholme(Saint-Louis)
Cap de Nouvelle-France
Baie Sugluk
Baie Déception
Hav
re D
ougl
as
Baie Wak
eham
BaieFisher
BaieJoy
BaieWhitley
Baie Korak
Diffusion : Ministère des Ressources naturelles et de la Faune
Géologie Ministère des Ressources naturelles et de la Faune,Géologie Québec 2007
1990
1997
Contacts géologiques de la demie orientaledes domaines Nord et Sud, de l'Antiforme deKovik et de l'Arc de Narsajuaq
Commission géologique du Canada, Cartes 1721A à 1735A
Cartes 1911A à 1914A
HydrographieMinistère des Ressources naturelles et de la Faune,Direction générale de l'information géographique 2002
Données numériques d'élévation Commission géologique du Canada, Dossier public 5117 2007
Le présent document n'a aucune portée légaleDépôt légal - Bibliothèque nationale du Québec© Gouvernement du Québec
* Les unités de la Province du Supérieur présentées sur cette carte sont décrites dans le Lexique stratigraphique des unités archéennes du nord-est de la Province du Supérieur (Simard, DV 2008-03).
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