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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

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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