Weeek 7 Flashcards

1
Q

thickness crust

A

6-7 km

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2
Q

thickness lithosphere

A

up to 100 km

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3
Q

melting starts at

A

50 km

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4
Q

extraction at mid ocean ridges

A

Melt runs into low-permeability barrier (lithosphere) → Melt is focused due to pressure gradients from flow.

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5
Q

ocean layer 1

A

sediments
0 to 0.5 km
Vp 1.7-2 km/ s

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6
Q

ocean layer 2a

A

Pillow basalt
0.5 km
2-5.5 km/ s

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7
Q

layer 2b

A

sheeted dyke basalt
1.5 km
6-76 km(s

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8
Q

layer 3a

A

Gabbro isotropic
5km
7 km/s

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9
Q

layer 3b

A

gabbro layered

same as 3a

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10
Q

layer 4a

A

Peridotite
Dunite, layered peridotitw
1.2 km
8 km/ s

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11
Q

layer 4b

A

isotropic peridotite

same as 4a

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12
Q

geophysical moho

A

betweeen layer 3b and 4a

so between gabbro and peridotite

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13
Q

petrological moho

A

between layer 4a and 4b so peridotite layers

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14
Q

Wadati Berioff Zone

A
earthquke line, deepest part
dipping planar (flat) zone of earthquakes that is produced by the interaction of a downgoing oceanic crustal plate with a continental plate.
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15
Q

when change in temp, depth is sqr root of age

A

this is not linear bcs as crust gets older it gets colder an denser so submerges

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16
Q

Viscosity definition

A

measure of the resistance of a material to flow or to deform permanently

17
Q

high viscosity means

A

high resistance to flow, will flow slow (syrup)

18
Q

low viscosity means

A

low resistance to flow, will flow fast ( water(

19
Q

viscosity n

A

n as greek letter eta for viscisuty

20
Q

viscosity depends on

A

mineralogy, composition, water, grain size, strain rate, T and P

21
Q

as temperature increases, n

A

decreases

22
Q

as preessure increses, n

A

increases

23
Q

n unit

A

in pascal per seconds

24
Q

What is a plate?

A

radi number is smaller than critical radius
cools via conduction
has earthquakes, deforms via brittle deformation ( so breaks not flows)

25
Q

geological boundary

brittle ductile transition

A

point where viscous and brittle strength meet or interchange

also where lithisphere ends

26
Q

lithosphere ends

A

brittle ductile transition of a . plate

27
Q

strentgh envelope

A

dreieck under brittle strength line and above viscous strentgh line