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The metamorphic basement is around 25 km thick, and the average thickness of the sedimentary cover is around 15 km.
Optical thickness of each mode in each layer (2 km thick) at 920 nm is represented.
The observed Bouguer gravity anomalies are explained by ∼10 km thick Granitic upper crust of 2.7 g/cm3; ∼10 km thick intermediate mid crust of 2.82 g/cm3; ∼15 km thick mafic lower crust of 2.91 g/cm3 density.
In the deep ocean there is a sedimentary layer that is about 1 km thick.
Underneath is the lower layer of the oceanic crust, which is about 4 km thick.
The subducting oceanic crust of the Huatung Basin is about 5 6 km thick.
Similar(10)
Case (1) assumes that deformation occurs only within the 1-km thick fracture zone.
For models RF3 and RF2, the elastic lithosphere is 115-km thick.
The laterally homogenous lithosphere consists of a bi-layer, 36-km-thick crust and 114-km-thick lithospheric mantle.
The bulk section exhibits a 15-km-thick arc crustal section.
The ∼ 3 km-thick Western Mirdita ophiolite (WMO) contains lherzolitic peridotites and gabbros overlain by basaltic pillow lavas, whereas the ∼ 12 km-thick Eastern Mirdita ophiolite (EMO) represents a Penrose-type oceanic crust with suprasubduction zone affinities.
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