Results 131 to 140 of about 5,189,165 (162)
Magmatic-hydrothermal fluid evolution of the tin-polymetallic metallogenic systems from the Weilasituo ore district, Northeast China. [PDF]
Gao X +6 more
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Deep time evolution of the Latitudinal Diversity Gradient: Insights from mechanistic models. [PDF]
Lorcery M +5 more
europepmc +1 more source
Apatite textural and geochemical insights into the petrogenesis of intrusive rocks. [PDF]
Li H +8 more
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Editorial: Paleo-Asian and Tethyan domains: magmatism, tectonics, mineralization, and geodynamics
Xijun Liu +5 more
doaj +1 more source
Abstract The early-stage subduction records of the Paleo-Asian ocean are poorly preserved in the eastern segment of the Central Asian Orogenic Belt (CAOB), which hinders constraints on the evolution of the whole CAOB. This study presents new age data and zircon Hf-O isotopes as well as bulk-rock geochemistry of the Wuxing mafic ...
Meng-Meng Cui +4 more
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Abstract The Central Asian Orogenic Belt (CAOB) was the result of long-lived multi-stage tectonic evolution, including Proterozoic to Paleozoic accretion and collision, Mesozoic intracontinental modification, and Cenozoic rapid deformation and uplift.
Keda Cai +4 more
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Marine and Petroleum Geology, 2021
Abstract Large Carboniferous petroleum systems exist in the Central Asian Orogenic Belt (CAOB), including the South Caspian and Junggar basins. In this study, we investigated one such petroleum system in the range belt by analyzing hydrocarbons in vein cements in the Daerbute fault zone that cuts Carboniferous strata in West Junggar, northwest China.
Jian Cao, Baoli Bian, Dongming Zhi
exaly +2 more sources
Abstract Large Carboniferous petroleum systems exist in the Central Asian Orogenic Belt (CAOB), including the South Caspian and Junggar basins. In this study, we investigated one such petroleum system in the range belt by analyzing hydrocarbons in vein cements in the Daerbute fault zone that cuts Carboniferous strata in West Junggar, northwest China.
Jian Cao, Baoli Bian, Dongming Zhi
exaly +2 more sources
Gondwana Research, 2016
Abstract The Dunhuang region is located in the east of the Tarim Craton and has long been considered as part of a Precambrian terrane of the Tarim or North China Craton. Aiming to further understand the tectonic evolution of the Dunhuang region and its relations with the adjacent tectonic units, this study is to investigate the metamafic rocks in the
Tao Zhu
exaly +2 more sources
Abstract The Dunhuang region is located in the east of the Tarim Craton and has long been considered as part of a Precambrian terrane of the Tarim or North China Craton. Aiming to further understand the tectonic evolution of the Dunhuang region and its relations with the adjacent tectonic units, this study is to investigate the metamafic rocks in the
Tao Zhu
exaly +2 more sources
Precambrian Research, 2017
Abstract An early extensive Neoproterozoic (ca. 900 Ma) continental magmatic arc system covering hundreds of kilometers has been reported to occur in the South Beishan Orogenic Belt (SBOB) and the Central Tianshan (CTA) in the southern Central Asian Orogenic Belt (CAOB).
Zhaochu Hu, Zhenyu He, Zeming Zhang
exaly +2 more sources
Abstract An early extensive Neoproterozoic (ca. 900 Ma) continental magmatic arc system covering hundreds of kilometers has been reported to occur in the South Beishan Orogenic Belt (SBOB) and the Central Tianshan (CTA) in the southern Central Asian Orogenic Belt (CAOB).
Zhaochu Hu, Zhenyu He, Zeming Zhang
exaly +2 more sources
Lithos, 2013
Abstract Zircon U–Pb ages, whole-rock geochemical and zircon Hf isotope data are reported for the Permian A-type quartz syenites–granites in western Tarim Block, Northwest China. Zircon U–Pb dating indicates these alkali plutons were emplaced at 270–277 Ma.
Haibo Zou, Zhang Chuan-Lin
exaly +2 more sources
Abstract Zircon U–Pb ages, whole-rock geochemical and zircon Hf isotope data are reported for the Permian A-type quartz syenites–granites in western Tarim Block, Northwest China. Zircon U–Pb dating indicates these alkali plutons were emplaced at 270–277 Ma.
Haibo Zou, Zhang Chuan-Lin
exaly +2 more sources

