Weeek 7 Flashcards
thickness crust
6-7 km
thickness lithosphere
up to 100 km
melting starts at
50 km
extraction at mid ocean ridges
Melt runs into low-permeability barrier (lithosphere) → Melt is focused due to pressure gradients from flow.
ocean layer 1
sediments
0 to 0.5 km
Vp 1.7-2 km/ s
ocean layer 2a
Pillow basalt
0.5 km
2-5.5 km/ s
layer 2b
sheeted dyke basalt
1.5 km
6-76 km(s
layer 3a
Gabbro isotropic
5km
7 km/s
layer 3b
gabbro layered
same as 3a
layer 4a
Peridotite
Dunite, layered peridotitw
1.2 km
8 km/ s
layer 4b
isotropic peridotite
same as 4a
geophysical moho
betweeen layer 3b and 4a
so between gabbro and peridotite
petrological moho
between layer 4a and 4b so peridotite layers
Wadati Berioff Zone
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.
when change in temp, depth is sqr root of age
this is not linear bcs as crust gets older it gets colder an denser so submerges
Viscosity definition
measure of the resistance of a material to flow or to deform permanently
high viscosity means
high resistance to flow, will flow slow (syrup)
low viscosity means
low resistance to flow, will flow fast ( water(
viscosity n
n as greek letter eta for viscisuty
viscosity depends on
mineralogy, composition, water, grain size, strain rate, T and P
as temperature increases, n
decreases
as preessure increses, n
increases
n unit
in pascal per seconds
What is a plate?
radi number is smaller than critical radius
cools via conduction
has earthquakes, deforms via brittle deformation ( so breaks not flows)