Results 241 to 250 of about 79,295 (351)
Abstract Three voluminous inflated lobate lava flow complexes on the distal rifts of Axial Seamount are much larger than other known flows in the global spreading system. Each complex is 65–100 km2, is up to 130 m thick, and is ∼3.0–4.6 km3, almost 100 times the volumes of historical Axial flows.
Jennifer B. Paduan +5 more
wiley +1 more source
The source-to-sink system in continental rift lacustrine basins of the Nantun Formation in X Sag of the Tamtsag Basin, Mongolia. [PDF]
Liu L +6 more
europepmc +1 more source
Sedimentary environments and their facies of the carbonate reservoir rocks : Conclusional review.
Kazukiyo Oshima
openalex +2 more sources
Abstract Subduction initiation often begins with slow, forced convergence, switches “on” catastrophically as the slab collapses into the mantle, and then evolves to steady‐state, self‐sustained sinking that drives global plate movements. Numerical models suggest that the collapse phase implies sudden weakening of the plate interface.
Alissa J. Kotowski +3 more
wiley +1 more source
Tectonoclimatic controls on Paleogene braided river delta evolution and petroleum systems in the Lenghu tectonic belt, northern Qaidam Basin. [PDF]
Gong L, Gai W, Gao X, Hou Z.
europepmc +1 more source
Abstract We present elemental geochemistry and multiple isotopic systematics (Re‐Os, Lu‐Hf, Sm‐Nd and Sr) for mantle peridotite xenoliths from Lashaine in northern Tanzania. We use the data to examine how the major Proterozoic tectono‐thermal events that affected the crust of the western Tanzanian craton are imprinted on the lithospheric mantle in the ...
Sheng‐Hua Zhou +6 more
wiley +1 more source
Geological and physicochemical characterization of Kobe Sorsa graphite deposit, Ethiopia. [PDF]
Emmiru BT, Tsegaye SG, Sahoo PR.
europepmc +1 more source
Research on Constrained Sedimentary Facies Reservoir by Well-seismic Inversion
Zhiwei Chen
openalex +1 more source
Abstract Martian carbonate‐bearing rocks are compelling targets for exploration because they preserve detailed records of past aqueous processes, climate, and habitability. The Margin unit in Jezero crater is a distinct olivine‐ and carbonate‐bearing unit stratigraphically underlying the western fan, lining the inner margin of the western crater rim ...
Alexander J. Jones +29 more
wiley +1 more source

