Results 211 to 220 of about 59,876 (275)
Abstract The Northeastern (NE) Tibet, as the front of plateau growth, widely absorbs northeastward extrusion, leading to significant uplift and forming a basin‐mountain tectonic framework. However, it remains unclear how the crust of NE Tibet deformed in response to the far‐field effects of the India‐Eurasia collision.
Ruo‐Jie Li +4 more
wiley +1 more source
Water-rich incipient melt of the deep upper mantle indicates locally preserved low-velocity zones above the 410 km discontinuity. [PDF]
Xie L +4 more
europepmc +1 more source
Abstract Coupled climate‐ice‐sheet modeling is still in its developing stage, and feedback processes between ice sheets and climate are still not yet fully understood. Here, we use simulations with a coupled climate‐ice‐sheet model to investigate teleconnections between Northern Hemispheric ice sheets and the Antarctic ice sheet (AIS) without direct ...
Pierre Testorf +3 more
wiley +1 more source
Superionicity of oxygen-deficient davemaoite and its impact on the deep-Earth oxidation cycle. [PDF]
Wang Z, He Y, Mao HK, Kim DY.
europepmc +1 more source
Large melt diversity at a mid-ocean ridge thermal low. [PDF]
Brunelli D +8 more
europepmc +1 more source
Missing molybdenum and the composition of the continental crust inferred from molybdenum isotopes. [PDF]
Tian Y +5 more
europepmc +1 more source
Mode of intracontinental mountain building controlled by lower crustal composition and mantle lithosphere depletion. [PDF]
Xu X +14 more
europepmc +1 more source
Plume-induced emissions of deep methane linked to the end-Guadalupian mass extinction. [PDF]
Liu SA, Xiong Z, Wu T, Zhao M.
europepmc +1 more source
Ultraslow mid-ocean ridges: ultra focused magma supply. [PDF]
Lin J, Zhang F, Zhou Z.
europepmc +1 more source
Mantle plumes, convection and decompression melting
Manglik, Ajai, Christensen, Ulrich R.
openaire +1 more source

