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Normal faults -rifted continental margins -form in extension -typical for continental and oceanic lithosphere -jargon (horsts, grabens, listric, detachment) -are they low-angle? -core complexes -Example: Basin and Range, the best of all -the way we think it works, mechanically -balancing cross-sections
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Normal faults -rifted continental margins -form in extension -typical for continental and oceanic lithosphere -jargon (horsts, grabens, listric, detachment)

Dec 20, 2015

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Page 1: Normal faults -rifted continental margins -form in extension -typical for continental and oceanic lithosphere -jargon (horsts, grabens, listric, detachment)

Normal faults-rifted continental margins

-form in extension

-typical for continental and oceanic lithosphere

-jargon (horsts, grabens, listric, detachment)

-are they low-angle?

-core complexes

-Example: Basin and Range, the best of all

-the way we think it works, mechanically

-balancing cross-sections

Page 2: Normal faults -rifted continental margins -form in extension -typical for continental and oceanic lithosphere -jargon (horsts, grabens, listric, detachment)

Can you spot the fault?

Page 3: Normal faults -rifted continental margins -form in extension -typical for continental and oceanic lithosphere -jargon (horsts, grabens, listric, detachment)

It’s low angle, but so are thrust faults:KEY: puts young (hanging wall) on old(footwall). The fault markers (slickenlinesEtc) are the same.

Page 4: Normal faults -rifted continental margins -form in extension -typical for continental and oceanic lithosphere -jargon (horsts, grabens, listric, detachment)

Terminology and mechanism.KEY ASPECTS:High-angle vs. low angle normal faulting; whichone generates more extension (S)? The formation of core complexesMajor detachment faults.How can we distinguish the low-angle normal faultingStyle from thrusting (if only geometry is available)?

Page 5: Normal faults -rifted continental margins -form in extension -typical for continental and oceanic lithosphere -jargon (horsts, grabens, listric, detachment)

Basin and Range- world’smost studied extensionalprovince-low-angle normal faulting prevails. Tibet-similar.

Page 6: Normal faults -rifted continental margins -form in extension -typical for continental and oceanic lithosphere -jargon (horsts, grabens, listric, detachment)
Page 7: Normal faults -rifted continental margins -form in extension -typical for continental and oceanic lithosphere -jargon (horsts, grabens, listric, detachment)
Page 8: Normal faults -rifted continental margins -form in extension -typical for continental and oceanic lithosphere -jargon (horsts, grabens, listric, detachment)
Page 9: Normal faults -rifted continental margins -form in extension -typical for continental and oceanic lithosphere -jargon (horsts, grabens, listric, detachment)

Breakaway zone; importance of a brittle-ductile transition

Page 10: Normal faults -rifted continental margins -form in extension -typical for continental and oceanic lithosphere -jargon (horsts, grabens, listric, detachment)

Inversion tectonics- normal faults become thrusts and inverse faults. A regional system formed in extension isforced to shorten.

How it might work

Page 11: Normal faults -rifted continental margins -form in extension -typical for continental and oceanic lithosphere -jargon (horsts, grabens, listric, detachment)
Page 12: Normal faults -rifted continental margins -form in extension -typical for continental and oceanic lithosphere -jargon (horsts, grabens, listric, detachment)

Important things about normal faults.

1. Fundamental to structure of continents and oceans.

Page 13: Normal faults -rifted continental margins -form in extension -typical for continental and oceanic lithosphere -jargon (horsts, grabens, listric, detachment)

Important things about normal faults.

2. Two different styles: the low-angle and high-angle.

Page 14: Normal faults -rifted continental margins -form in extension -typical for continental and oceanic lithosphere -jargon (horsts, grabens, listric, detachment)

Important things about normal faults.

3. Can take up as much extension as compressional orogens shorten.

Page 15: Normal faults -rifted continental margins -form in extension -typical for continental and oceanic lithosphere -jargon (horsts, grabens, listric, detachment)

Important things about normal faults.

4. You live in the most famous (and perhapsmost important extensional region-the B&R).

Page 16: Normal faults -rifted continental margins -form in extension -typical for continental and oceanic lithosphere -jargon (horsts, grabens, listric, detachment)

Important things about normal faults.

5. Extension is accompanied by big-time sedimentation-important for oil formation.

Page 17: Normal faults -rifted continental margins -form in extension -typical for continental and oceanic lithosphere -jargon (horsts, grabens, listric, detachment)

Important things about normal faults.

1. Fundamental to structure of continents and oceans.2. Two different styles: the low-angle and high-angle.3. Can take up as much extension as compressional orogens shorten.4. You live in the most famous (and perhapsmost important extensional region-the B&R).5. Extension is accompanied by big-time sedimentation-important for oil formation.