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Divergent boundary Transform fault Convergent boundary Three types of plate boundaries Fig. 1
49

Divergent boundary Transform fault Convergent boundary Three types of plate boundaries Fig. 1.

Dec 16, 2015

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Perla Ketcham
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Page 1: Divergent boundary Transform fault Convergent boundary Three types of plate boundaries Fig. 1.

Divergent boundary

Transform fault

Convergent boundary

Three types of plate boundaries

Fig. 1

Page 2: Divergent boundary Transform fault Convergent boundary Three types of plate boundaries Fig. 1.

Morphologies, seismicity and plate boundaries

Mid-ocean ridge

Fracture zone

Deep-sea trench

Fig. 2

Page 3: Divergent boundary Transform fault Convergent boundary Three types of plate boundaries Fig. 1.

Benard (1901)

Downwelling

Upwelling

Planform of thermal convection

Fig. 3

Page 4: Divergent boundary Transform fault Convergent boundary Three types of plate boundaries Fig. 1.

Bercovich (1995)

Fig. 4

Poloidal component

Toroidal component

Surface velocities

Page 5: Divergent boundary Transform fault Convergent boundary Three types of plate boundaries Fig. 1.

Earthquake = Faulting

Normal fault

Fig. 5Modified from Paterson (1958)

Page 6: Divergent boundary Transform fault Convergent boundary Three types of plate boundaries Fig. 1.

δ:

λ:

φ−ψ:

φ: ëñå¸

åXäp

ÉXÉäÉbÉvÉxÉNÉgÉãÇÃï˚å¸

Ç∑Ç◊ÇËäpÅAÉåÉCÉN

φ

u:

u

λ Ç∑Ç◊ÇËó 

strike

dip angle

rake or slip angle

amount of slip

slip vector direction

Fault parameters of an earthquake

Fault plane

Fig. 6

ψ

usinλcosδ/ucosλ = tan( ψ)

cosδtanλ = tan( ψ)

Page 7: Divergent boundary Transform fault Convergent boundary Three types of plate boundaries Fig. 1.

A

B

C

D

(a)

Fig. 7a

Focal mechanism of an earthquake

Page 8: Divergent boundary Transform fault Convergent boundary Three types of plate boundaries Fig. 1.

(b)

A

B C

D

Fig. 7b

Fault plane

Auxiliary plane

Page 9: Divergent boundary Transform fault Convergent boundary Three types of plate boundaries Fig. 1.

Fig. 8

Slip vector and auxiliary plane

Page 10: Divergent boundary Transform fault Convergent boundary Three types of plate boundaries Fig. 1.

Age distribution of ocean floor

Sclater et al. (1981)Fig. 9

Page 11: Divergent boundary Transform fault Convergent boundary Three types of plate boundaries Fig. 1.

4

6

km

4000 2000 6000 km

Tonga Trench

East Pacific Rise

Ocean floor topography profile

Fig. 10

Page 12: Divergent boundary Transform fault Convergent boundary Three types of plate boundaries Fig. 1.

Formation of Oceanic Crust

Partial melting

MeltBasalt

Gabbro, Cumulates

Detrick et al. (1987)

Moho

Fig. 11

M.O.R.

Page 13: Divergent boundary Transform fault Convergent boundary Three types of plate boundaries Fig. 1.

T

P

Ts

Tm

Decompressional melting

Fig. 12

Asthenosphere

Melting temperature

Start of melting

Page 14: Divergent boundary Transform fault Convergent boundary Three types of plate boundaries Fig. 1.

Magnetic anomaly stripes

Atlantic

Spreading axis

Fig. 13

Cox et al. (1967)

Page 15: Divergent boundary Transform fault Convergent boundary Three types of plate boundaries Fig. 1.

History of magnetic reversals

Harland et al. (1982) Fig. 14

Page 16: Divergent boundary Transform fault Convergent boundary Three types of plate boundaries Fig. 1.

RIDGE Planning Office(1989)

Basalts are altered (metamorphosed) by hydrothermal circulations.

Fig. 15

MOR activities at different spatial scales

Page 17: Divergent boundary Transform fault Convergent boundary Three types of plate boundaries Fig. 1.

Sykes (1967)

Normal fault-type focal mechanisms

Atlantic

Fig. 16

Page 18: Divergent boundary Transform fault Convergent boundary Three types of plate boundaries Fig. 1.

Normal Faulting

Macdonald (1982) Fig. 17

km

Page 19: Divergent boundary Transform fault Convergent boundary Three types of plate boundaries Fig. 1.

M.O.R.

Transform fault

Fracture zone

Plate APlate B

M.O.R.

Fig. 18

C

D

Ridge-ridge transform fault

Page 20: Divergent boundary Transform fault Convergent boundary Three types of plate boundaries Fig. 1.

Transform faults

Fig. 19

Atlantic

Fracture zone

Page 21: Divergent boundary Transform fault Convergent boundary Three types of plate boundaries Fig. 1.

Delong et al. (1979)

Fig. 20

Fracture zone

Page 22: Divergent boundary Transform fault Convergent boundary Three types of plate boundaries Fig. 1.

Focal Mechanisms

Engeln et al. (1986)

Fig. 21

Page 23: Divergent boundary Transform fault Convergent boundary Three types of plate boundaries Fig. 1.

Continental rifting and sea-floor spreading

Africa

S. America

Atlantic

Fig. 22

Sibuet & Mascle (1978)

Page 24: Divergent boundary Transform fault Convergent boundary Three types of plate boundaries Fig. 1.

L

l g

MOR

MOR

Transform

l

Fig. 23

Energy discippation

Page 25: Divergent boundary Transform fault Convergent boundary Three types of plate boundaries Fig. 1.

Trench-trench transform

Fig. 24

Page 26: Divergent boundary Transform fault Convergent boundary Three types of plate boundaries Fig. 1.

Trench-trench type transform fault

North Fiji Basin

TongaVanuatu

Fig. 25

Page 27: Divergent boundary Transform fault Convergent boundary Three types of plate boundaries Fig. 1.

Two types of convergent boundaries

Subduction zone Collision zone

Fig. 26

Page 28: Divergent boundary Transform fault Convergent boundary Three types of plate boundaries Fig. 1.

Subduction zone

Indian Ocean

Fig. 27

Page 29: Divergent boundary Transform fault Convergent boundary Three types of plate boundaries Fig. 1.

Fig. 28

Backarc Forearc

Accretionary prism

Outer-rise

Outer trenchslope

Backarc basin Forearcbasin

Inner trenchslope

Volcanic front

Karig (1974)

Tectonic elements in the subduction zone

Page 30: Divergent boundary Transform fault Convergent boundary Three types of plate boundaries Fig. 1.

Fig. 29

ÅúÅú

Åú

Åú

ÅúÅú

Åú

ÅúÅú

Åú

Åú

ÅúÅú

Åú

100 km

Youngest brothersEldest brothers

Middle brothers

Upper plate

Trench

Three brothers: earthquakes in subduction zones

Page 31: Divergent boundary Transform fault Convergent boundary Three types of plate boundaries Fig. 1.

Eldest brother: 1994 Sanriku (Ms 7.6)

Nakayama & Takeo (1997) Fig. 30

Page 32: Divergent boundary Transform fault Convergent boundary Three types of plate boundaries Fig. 1.

110 120 130 140 150 16020

30

40

50

60

Pacific

Okhotsk

Japan Sea

Phil. Sea

Amuria

EurasiaN. America

Wei & Seno (1989)

Slip vectors

Fig. 31

Page 33: Divergent boundary Transform fault Convergent boundary Three types of plate boundaries Fig. 1.

* = - p

Effective stress

w

Fig. 32

Lubrication by pore fluid pressure

Page 34: Divergent boundary Transform fault Convergent boundary Three types of plate boundaries Fig. 1.

Seafloor topography in the outer-rise region

Fig. 33

Cardwell et al. (1976)

Page 35: Divergent boundary Transform fault Convergent boundary Three types of plate boundaries Fig. 1.

Seno and Yamanaka (1996)

Trench – Outer rise earthquakes

Fig. 34

●: compression○: tension

Seno and Gonzalez (1987)

Compression

Tension

Page 36: Divergent boundary Transform fault Convergent boundary Three types of plate boundaries Fig. 1.

Seno and Yamanaka (1996)

Age/depth of outer-rise earthquakes

Depth

Black: compression

White: tension

Fig. 35

Age of the plate (Ma)

Page 37: Divergent boundary Transform fault Convergent boundary Three types of plate boundaries Fig. 1.

Matsuzawa et al. (1986)

Intermediate-depth earthquakes: Northern Honshu double seismic zone

Fig. 36

Page 38: Divergent boundary Transform fault Convergent boundary Three types of plate boundaries Fig. 1.

Bonin arcDeep seismicity

van der Hilst & Seno (1993)

Fig. 37

Page 39: Divergent boundary Transform fault Convergent boundary Three types of plate boundaries Fig. 1.

Dehydration embrittlement: Serpentinite

Raleigh & Paterson (1965)

Fig. 38

Page 40: Divergent boundary Transform fault Convergent boundary Three types of plate boundaries Fig. 1.

(a) Cold slab type (b) Hot slab type

Dehydration from crust

Dehydration from crust

Dehydration from serpentine

Dehydration from serpentine

Dehydration locus for slab seismicity

Yamasaki & Seno (2003)Fig. 39

Page 41: Divergent boundary Transform fault Convergent boundary Three types of plate boundaries Fig. 1.

Active faults in Japan

Fig. 40

Page 42: Divergent boundary Transform fault Convergent boundary Three types of plate boundaries Fig. 1.

Fault-types of activefaults in Japan

Huzita (1980)

Reverse

Strike-slip

Normal

Fig. 41

Page 43: Divergent boundary Transform fault Convergent boundary Three types of plate boundaries Fig. 1.

Volcanoes in Japan

Volcanic front

Fig. 42

Page 44: Divergent boundary Transform fault Convergent boundary Three types of plate boundaries Fig. 1.

Accretion: Offscarping at the toe of the trench

Seely et al. (1974)

Fig. 43

Page 45: Divergent boundary Transform fault Convergent boundary Three types of plate boundaries Fig. 1.

Accretionary prism at the Nankai Trough

Kuramoto et al. (2000)

Trough axis

Decollement

Fig. 44

Page 46: Divergent boundary Transform fault Convergent boundary Three types of plate boundaries Fig. 1.

Geological terranes of Japan

Fig. 45Y. Saito (unpublished material)

Page 47: Divergent boundary Transform fault Convergent boundary Three types of plate boundaries Fig. 1.

Subduction zone

Collision zone

Fig. 46

Page 48: Divergent boundary Transform fault Convergent boundary Three types of plate boundaries Fig. 1.

Molnar (1984)

Himalayas

300 km

Himalayan Frontal Thrust Indus-Zangpo Suture Zone

Fig. 47

Page 49: Divergent boundary Transform fault Convergent boundary Three types of plate boundaries Fig. 1.

Tapponnier et al. (1982)Fig. 48