Results 211 to 220 of about 61,955 (243)
Abstract Reliable prediction of earthquakes and rock mass failure has long been hampered by a fundamental trade‐off: achieving both a long warning window and high prediction accuracy. Physical models, such as the failure forecast method (FFM) based on the time‐reversed Omori law, can provide longer warning windows but are sensitive to data noise and ...
Jian‐Zhi Zhang +4 more
wiley +1 more source
Paleoarchean deep crustal hydration and oxidation induced by subduction-driven water recycling. [PDF]
Zhou D +7 more
europepmc +1 more source
Abstract The South Pacific Ocean (SPO) hosts diverse biogeographical environments including the productive Peru‐Chile upwelling region and ultra‐oligotrophic subtropical gyre; however, vast areas are understudied regarding the cycling of dissolved calcium (Ca) and strontium (Sr), and distribution of major biomineral‐forming pelagic marine organisms ...
Edel M. O'Sullivan +7 more
wiley +1 more source
Petrological and geochemical characterization of Abu Murrat syn-orogenic I-type and post-orogenic A-type neoproterozoic granitoids, North Eastern Desert, Egypt. [PDF]
El-Awady A +4 more
europepmc +1 more source
Abstract Oceanic Core Complexes (OCCs) in back‐arc basins are not as thoroughly investigated, and their termination processes remain poorly understood. The Godzilla Megamullion is the largest known ceased OCC on Earth, yet magmatic and hydrothermal records from its termination are lacking.
Han‐Tao Chi +3 more
wiley +1 more source
Contemporaneous mobile- and stagnant-lid tectonics on the Hadean Earth. [PDF]
Valley JW +11 more
europepmc +1 more source
Abstract Oceanic lithosphere is continuously destroyed by subduction, challenging our ability to develop tectonic reconstructions. One way to tackle this problem is to examine relics of once‐consumed oceanic domains preserved along convergent margins. In the New England Orogen (eastern Australia), disrupted exposures of ultramafic rocks loosely define ...
J. A. Pasco +4 more
wiley +1 more source
Arc magma formation through the fluid-fluxed mélange melting in subduction zones. [PDF]
Zhang W +4 more
europepmc +1 more source
Anatomy of a post-subduction collision. [PDF]
Şengül Uluocak E +3 more
europepmc +1 more source
Phengite-mediated fluorine and chlorine fluxes from subduction zones to the deep mantle. [PDF]
Liu Y, Wang Y, Chen C, Gao M, Xu YG.
europepmc +1 more source

