Results 171 to 180 of about 13,835 (224)

Weak mantle wedge causes mantle exhumation punctuated with discrete oceanic crust in the Tyrrhenian basin. [PDF]

Nat Commun
Su H, Leng W, Liao J, Brune S.
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Seismic evidence for melt-rich lithosphere-asthenosphere boundary beneath young slab at Cascadia. [PDF]

Nat Commun
Wang X, Chen L, Wang K, Chen QF, Zhan Z, Yang J.   +5 more
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Multilevel transcrustal magmatic system beneath the Geysers-Clear Lake area. [PDF]

Proc Natl Acad Sci U S A
Li T, Wu S, Tong P.
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Subducted carbon weakens the forearc mantle wedge in a warm subduction zone. [PDF]

Nat Commun
Oyanagi R, Okamoto A.
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Uplift of the Tibetan Plateau driven by mantle delamination from the overriding plate. [PDF]

Nat Geosci
Xie Y, Balázs A, Gerya T, Xiong X.
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Optimal truss design with MOHO: A multi-objective optimization perspective. [PDF]

PLoS One
Mashru N, Tejani GG, Patel P, Khishe M.
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Magnetotelluric evidence for the deep causes of different eruptive styles of Changbaishan Tianchi and Longgang volcanoes. [PDF]

Sci Rep
Zhao L, Zhan Y, Kiyan D, Xu J, Hu Y, Tang J, Sun X, Wang Q, Cao C.   +8 more
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Gravity, geoid, isostasy and moho depth in Ross Sea Antarctica

, 1997
Velicogna, I, Marson, I, Stoka, M, Coren, F, Zanolla, C   +4 more
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Moho depth and crustal velocities from the Bosporus to S.E. Asia

, 2012
W. Stolk, Mikhail Kaban, S. A. P. L. Cloetingh   +2 more
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The Moho depth map of the Antarctica region

Tectonophysics, 2013
Abstract Different tectonic units cover the Antarctic territory: platform, orogens and depression structures. This structural variability is reflected both in thickness and physical properties of the crust. We present a new Moho map for the Antarctica, derived from geophysical data selected from the literature.
A. Baranov, A. Morelli
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