Results 211 to 220 of about 127,950 (297)
Abstract The role of sub‐arc mantle lithosphere in the build‐up of a batholith is an outstanding issue that is still not well resolved. Lamproite is a mantle‐derived magmatic rock that provides a window to learn the composition and the enrichment processes of subcontinental lithospheric mantle (SCLM).
Y. H. Tian +4 more
wiley +1 more source
Transition towards plate tectonics tracked in the metamorphic signature of Neoarchean synmagmatic transpression. [PDF]
Zibra I +4 more
europepmc +1 more source
Growth and Chemical Evolution of the Kohistan Arc Crust, Northern Pakistan, Western Himalayas
Abstract Fossil arcs which expose the middle‐lower crust have the potential to shed light on active arc processes because magmatic rocks from the entire history of the arc can be examined. We present new geochemical data from the middle crust of the Kohistan Arc and use existing geochemical and geochronological literature data from this arc to ...
Paul Sotiriou +2 more
wiley +1 more source
Experimental evidence supporting a long-lived magma layer at the Martian core–mantle boundary
Pierru R +9 more
europepmc +1 more source
Tunable Magnetism and Intrinsic Exchange Bias in Al-Substituted Terbium Iron Garnet. [PDF]
Shiino T +3 more
europepmc +1 more source
Abstract It is recognized that mantle plumes play a direct role in generating regional uplift and producing immense volumes of basaltic magmatism, both of which can influence paleoclimate. The Icelandic Plume, beneath the North Atlantic Ocean, is of particular importance due to its size and position at a significant paleoceanographic gateway.
Nicky White +5 more
wiley +1 more source
In-sensor analog optoelectronic processing of concurrent event and memory signals for dynamic vision sensing. [PDF]
Kim Y +12 more
europepmc +1 more source
Slab Gap‐Related Intraplate Magmatism as a Proxy of Maximum Flat Slab Extent in Patagonia
Abstract Establishing the frontal extent of ancient flat subduction events from the geologic record can be challenging. This difficulty arises because magmatic activity in the arc typically ceases during complete slab flattening, and other meaningful proxies are usually absent. To address this issue, we examine early Paleocene intraplate magmatic units
C. R. Navarrete +3 more
wiley +1 more source
Iron disproportionation in peridotite fragments from the mantle transition zone. [PDF]
Pan F +10 more
europepmc +1 more source

