Results 131 to 140 of about 372,925 (229)
Towards a definition of a spatial geochemical compatibility: workflow, validation, and application
M. V. Zuccolini+2 more
semanticscholar +1 more source
Abstract The Great Meteor seamounts are located in the eastern Atlantic Ocean, about 750 km south of the Azores. Conjugate to the Corner seamounts in the western Atlantic Ocean, it has been suggested they formed at the same hotspot that generated the New England Seamount chain.
A. B. Watts, I. Grevemeyer
wiley +1 more source
The Sporadic Fluvial Regime of Pliva Vallis, the Outlet Valley of Jezero Crater Lake, Mars
Abstract In situ and orbital observations have suggested that Jezero crater (field site for the Mars 2020 Perseverance rover) once hosted a paleolake fed by two inlet valleys. An outlet valley, Pliva Vallis, is present on the eastern rim of the crater and raises the question of whether the lake system operated as an open basin or as a closed basin ...
J. Villette+4 more
wiley +1 more source
PSV10: A Global Data Set for 0-10 Ma Time-Averaged Field and Paleosecular Variation Studies [PDF]
Coe R. S.+5 more
core +2 more sources
A Compact, Low‐Cost Sensing System to Enable Distributed Measurements of Urban Tree Transpiration
Abstract Urban trees reduce air temperature and alleviate urban heat island effects through shading and transpiration, making them crucial components of climate adaptation strategies. Understanding their transpiration rates and patterns can give new insights into their response to climate stress, yet traditional sap‐flux measurements—which often ...
Xiating Chen+4 more
wiley +1 more source
Abstract Post‐collisional mafic rocks not only record geodynamic processes at the end of the orogenic cycle but also retain various clues regarding preceding interactions between subducted slabs and mantle wedges. However, the latter and related indicators have often been overlooked; in particular, how the continental crust interacts with the mantle in
Xiangyu Gao+7 more
wiley +1 more source
Abstract We modeled the evolution of the terrestrial Magma Ocean using the short‐lived 182Hf‐182W isotope system (t1/2 = 8.9 Myr) in a multi‐reservoir early Earth. We start with a chondritic Earth at T0 = 4.567 Ga. Core segregates and attains its present‐day mass, W elemental and isotopic (182W/184W) composition by the end of core formation (TCF).
Seema Kumari, Ramananda Chakrabarti
wiley +1 more source
Polycyclic aromatics in the Chang'E 5 lunar soils. [PDF]
Zhong G+18 more
europepmc +1 more source
Abstract Using our recently developed X‐ray diffraction based force constants approach, we have determined the equilibrium Si isotope fractionation between omphacite/garnet, quartz/kyanite, and quartz/zircon at temperatures relevant to the petrogenesis. We find that Na strongly affects the Si isotope fractionation between omphacite and garnet.
Dongzhou Zhang+4 more
wiley +1 more source
Sources and processes in arc magmatism: the crucial role of water [PDF]
Elburg, Marlina
core +1 more source