Results 181 to 190 of about 3,272 (233)
Abstract This study integrates new zircon U–Pb ages, zircon εHf(t)–δ18O isotopic data, and whole‐rock geochemistry to refine the temporal and spatial framework of magmatism in the southern Northern Andes (SNA) from ∼65 to 6 Ma. The San Lucas, Catamayo, Portachuela, and Gonzanamá batholiths and magmatic suites, along with Late Miocene plutons, display ...
J. Iglesias +14 more
wiley +1 more source
Intraplate deformation of Gondwana terranes and implications for the Wilson Cycle. [PDF]
Fonseca A, De Grave J.
europepmc +1 more source
Oxygen Isotopic Composition of Miocene Meteoric Water (δ18Ow) in Alpine Foreland Basins
Abstract The reconstructed stable oxygen isotopic composition of meteoric water (δ18Ow) is widely used for paleoclimate reconstructions. Understanding past environmental factors that drove changes in δ18Ow is essential for interpreting past climate conditions.
Armelle Ballian +6 more
wiley +1 more source
Redox chemistry of early Earth and the origin of life. [PDF]
Moldogazieva NT +3 more
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Complex Fault Systems and Basin Evolution of the Bonan Area, Eastern China: Effects on the Sedimentation and Distribution of Source Rocks. [PDF]
Wang F +8 more
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Large-scale crustal growth driven by LIP magmatism during the Paleoproterozoic. [PDF]
Simões MS +6 more
europepmc +1 more source
A mantle assist for the early geodynamo and planetary shielding. [PDF]
Tarduno JA.
europepmc +1 more source
Archean rifts and triple-junctions revealed by gravity modeling of the southern Superior Craton. [PDF]
Galley C +4 more
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Science, 2008
Although it is commonly assumed that subduction has operated continuously on Earth without interruption, subduction zones are routinely terminated by ocean closure and supercontinent assembly. Under certain circumstances, this could lead to a dramatic loss of subduction, globally.
Paul G, Silver, Mark D, Behn
openaire +2 more sources
Although it is commonly assumed that subduction has operated continuously on Earth without interruption, subduction zones are routinely terminated by ocean closure and supercontinent assembly. Under certain circumstances, this could lead to a dramatic loss of subduction, globally.
Paul G, Silver, Mark D, Behn
openaire +2 more sources

