Results 181 to 190 of about 379,430 (254)
Mode of intracontinental mountain building controlled by lower crustal composition and mantle lithosphere depletion. [PDF]
Xu X +14 more
europepmc +1 more source
The Depositional Record, Volume 12, Issue 4, September 2026.
Jaco H. Baas +2 more
wiley +1 more source
Brine Pool Microbes Enrich Metalliferous Sediments in Salt Giant Basins
Abstract We report the discovery of an extinct deep‐sea brine pool in the Red Sea's Hume Deep, providing evidence that rift‐shoulder pools are ephemeral on millennial timescales, and that the microbially‐enriched metalliferous deposits produced during the pool's active phase persist into the stratigraphic record.
Morgan I. Chakraborty +11 more
wiley +1 more source
A more reduced mantle beneath the lunar South Pole-Aitken basin. [PDF]
Zhang H +16 more
europepmc +1 more source
Abstract The Gyeonggi Massif is one of the major Precambrian basements in the Korean Peninsula where Paleoproterozoic orthogneiss and paragneiss were widely exposed. In this study, newly identified Rhyacian to Orosirian meta‐igneous rocks from the northwestern Gyeonggi Massif (Soyeonpyeongdo and Ganghwado areas) were investigated to elucidate their ...
Seung Hwan Lee +5 more
wiley +1 more source
Origin and evolution of fluids and heatflow in geothermal systems of Indus River Basin (IRB), India. [PDF]
Jeelani G +4 more
europepmc +1 more source
Investigating Layered Cratonic Lithosphere in the Fennoscandian Shield
Abstract Cold, thick, and chemically depleted lithosphere with high seismic velocity and low attenuation characterizes continental cratons. However, discrepancies between xenolith‐based thermal constraints and those inferred from surface‐wave seismic models, together with the widespread observation of mid‐lithosphere discontinuities, challenge the ...
Yiran Huang +2 more
wiley +1 more source
Sulfur-enriched sub-arc fluids drive deep sulfur cycling in subduction zones. [PDF]
Tan DB +10 more
europepmc +1 more source
Abstract Subglacial sedimentary basins in Antarctica are hypothesized to modulate ice flow and biogeochemical cycles via groundwater and geothermal feedbacks, yet their properties remain poorly constrained. Here, we present a joint quantitative analysis of new magnetotelluric (MT) data acquired at Thwaites Glacier (TG) and WAIS Divide, alongside legacy
Siobhan F. Killingbeck +8 more
wiley +1 more source
Felsic hydrothermal deposit formation by chalcophile metal concentration through mafic recharge and fluid-mediated sulfide dissolution. [PDF]
Liu Y +6 more
europepmc +1 more source

