FEATURES OF DETERMINATION OF MODERN GAS MIGRATION IN THE UPPER LAYERS OF THE LITHOSPHERE
N.V. Vergelska, І.М. Skopychenko
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Lithosphere delamination with foundering of lower crust and mantle caused permanent subsidence of New Caledonia Trough and transient uplift of Lord Howe Rise during Eocene and Oligocene initiation of Tonga-Kermadec subduction, western Pacific [PDF]
Rupert Sutherland +12 more
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Silica is unlikely to be soluble in upper crustal carbonatite melts
Michael Anenburg, Tibor Guzmics
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Using combined seismic refraction/wide-angle reflection method project Alp 2002 explored the contact zone between South-Eastern Alps, Dinarides and Pannonian basin.
Andrej Gosar
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Comment on “Is there a genetic relationship between selected regional joints and contemporary stress within the lithosphere of North America?” [PDF]
Adrian E. Scheidegger
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Geodynamic evolution of Upper Cretaceous Zagros ophiolites: formation of oceanic lithosphere above a nascent subduction zone [PDF]
Hadi Shafaii Moghadam, Robert J. Stern
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Evolution Characteristics through Thermo-Rheological Lithosphere of the Liaonan Metamorphic Core Complex, Eastern North China Craton [PDF]
Haonan Gan +3 more
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Role of asthenosphere and lithosphere in the genesis of Late Cenozoic basaltic rocks from the Rio Grande Rift and adjacent regions of the southwestern United States [PDF]
Frank Perry +2 more
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Investigation of the Central Adriatic lithosphere structure with the AlpArray-CASE seismic experiment [PDF]
Irene Molinari +10 more
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The Archean Superior craton was formed by the assemblage of continental and oceanic terranes at ∼2.6 Ga. The craton is surrounded by multiple Proterozoic mobile belts, including the Paleoproterozoic Trans‐Hudson Orogen which brought together the Superior
Riddhi Dave +3 more
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