Results 111 to 120 of about 315,024 (237)
Reconstruction of Rock Uplift in South‐Central Germany Since Late Mesozoic Times
Abstract Rock uplift and denudation act as first‐order controls on geological processes that influence atmospheric and ocean composition, and landscape‐forming processes. However, estimating rock uplift rates remains challenging due to the temporal averaging of rates calculated from individual thermo‐ or geochronologic systems.
Thomas Bernard +7 more
wiley +1 more source
Melt Production and Volatile Release From Thermochemical Mantle Plumes
Abstract Mantle plumes are thought to generate Large Igneous Provinces (LIPs), the largest outpourings of lava in the geologic record, which are associated with long‐lasting climatic warming events and mass extinctions. However, the controls on mantle degassing by plumes remain poorly constrained.
Qianyi Lu +2 more
wiley +1 more source
Diamond preservation in the lithospheric mantle recorded by olivine in kimberlites. [PDF]
Giuliani A +8 more
europepmc +1 more source
Abstract Studies of postseismic creep often infer a strong reduction in upper‐mantle viscosity after large earthquakes, yet the microphysical mechanism responsible for this behavior remains subject of debate. Here, we present new gas‐medium apparatus experiments at 1100–1200°C on pre‐dried, annealed Åheim dunite (grain size of 400 μ ${\upmu }$m ...
D. Hein, L. N. Hansen, A. Dillman
wiley +1 more source
The Lewisian Gneiss Complex of NW Scotland represents the eastern margin of the North Atlantic Craton. It comprises mid-late Archaean tonalite-trondhjemite-granodiorite gneisses that were metamorphosed and deformed during the Late-Archaean and ...
Hannah S. R. Hughes +6 more
semanticscholar +1 more source
Abstract Variations in melt supply can shift slow and ultraslow ridges between magmatic and tectonic accretion modes, but whether this effect persists at Earth's slowest‐spreading ridge remains unclear. The eastern Gakkel Ridge provides a critical test because it spreads at only ∼6–10 mm/yr yet shows anomalously strong magmatism.
Chaojin Huang +4 more
wiley +1 more source
Destruction and regrowth of lithospheric mantle beneath large igneous provinces. [PDF]
Stephenson SN, Ball PW, Richards FD.
europepmc +1 more source
Abstract The timing of Cenozoic deformation in the East Kunlun Mountains, northern Tibet, is crucial for understanding plateau growth but remains disputed due to the scarcity of direct chronological constraints on specific tectonic structures. Here, we present a high‐density‐sampling magnetostratigraphic record from the Xiaohongshan section, interior ...
Leyi Li +3 more
wiley +1 more source
Oceanic lithospheric mantle beneath the continental crust of the Chinese Altai
Although subduction-accretion is proposed as a major regime in making new continental crust, how the lithospheric mantle forms remains unclear. Formed after the closure of the Palaeo-Asian Ocean, the Ashele basalt shows normal mid-ocean ridge basalt (N ...
Chao Yuan +18 more
core +1 more source
Potassium distribution and isotope composition in the lithospheric mantle in relation to global Earth's reservoirs. [PDF]
Ionov DA, Wang K.
europepmc +1 more source

