Results 141 to 150 of about 29,339 (247)
Progress in geochronology: not only timing, but also rate. [PDF]
Li XH.
europepmc +1 more source
Gomez aminozones from Wehmiller, 2013, Quaternary Geochronology
Histogram of D/L values for the four aminozones found in the units exposed at Gomez Pit, Virginia Beach, VA. From Wehmiller, 2013, Quaternary Geochronology 16 (3-20)
Wehmiller, John F.
core
Abstract Precambrian supercontinent reconstructions largely rely on robust geological constraints. Among these, the basin affinities recorded by Precambrian sedimentary fragments preserved in orogenic belts provide critical evidence for resolving the paleogeographic configurations of microcontinents and continental blocks.
Yongcheng Li +14 more
wiley +1 more source
Ancient landscape evolution tracked through cosmogenic krypton in detrital zircon. [PDF]
Dröllner M +5 more
europepmc +1 more source
Abstract The North Altyn ophiolitic belt was formed by the subduction–closure of the Altyn segment of the Proto–Tethys Ocean and recorded the accretion of Tarim to northern Gondwana, but the timing of initial subduction and detailed tectonic transition processes remain poorly constrained. This study reports the oldest Phanerozoic magmatic record of 537
Long Chen +8 more
wiley +1 more source
Carbon and nitrogen isotope characterization of imported coals in South Korea
Eui-Kuk Jeong +8 more
doaj +1 more source
Method development with LA-ICP-MS in U-Pb geochronology using design of experiment. [PDF]
Caner M, Tunç M, Sunal G, Sarıkaya MA.
europepmc +1 more source
Role of Post‐Collisional Magmatism in Continental Growth and Reworking Since the Late Archean
Abstract The mechanisms responsible for the formation and compositional evolution of continental crust remain central questions in Earth science. Post‐collisional magmatism is widely preserved in the continental record; however, its contribution to crustal growth may be underestimated because enriched isotopic signatures obscure juvenile mantle input ...
Dongjian Ouyang +4 more
wiley +1 more source
Trace elements in the silicate minerals of the Borodino Meteorite (Н5)
Major (EPMA) and trace (SIMS) element geochemistry in olivine, low-Са pyroxene and mesostasis from porphyritic and barred chondrules, as well as the pyroxene-olivine aggregate and matrix of equilibrated ordinary Borodino chondrite (Н5) is discussed. No
Kristina G. Sukhanova
doaj
Re-Os geochronology for sulfides and organic-rich sediments. [PDF]
Li Y, Glorie S, Selby D.
europepmc +1 more source

