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The Petrogenesis of the Permian Podong Ultramafic Intrusion in the Tarim Craton, Western China: Constraints from C-He-Ne-Ar Isotopes
Published 2019-01-01“…The results show that olivine, pyroxene, and plagioclase minerals in the Podong intrusion have variable δ13C of CO2 (-24.5‰ to -3.2‰). The CH4, C2H6, C3H8, and C4H10 hydrocarbon gases show normal or partial reversal distribution patterns of carbon isotope with carbon number and light δ13C1 value of CH4, indicating the hydrocarbon gases of biogenic origin. …”
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TÉCNICAS PERUANAS MILENARIAS DE MANEJO DE LADERAS: SU APLICACIÓN EN EL CAJÓN DE ARROYO VARVARCO SUPERIOR
Published 2003-12-01Get full text
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Fibrina rica en plaquetas y leucocitos en abordajes endonasales endoscópicos
Published 2024-01-01Get full text
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O-GlcNAcylated FTO promotes m6A modification of SOX4 to enhance MDS/AML cell proliferation
Published 2025-01-01Get full text
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