Geochronology and petrogenesis of granitic rocks in Gangdese batholith, southern Tibet

Based on petrological and geochemical characteristics such as rock assemblage, petrogeochemistry, Sr-Nd isotope, zircon U-Pb age, and Hf isotope, we studied geochronological framework, magma types, source characters, and petrogenesis of different stages of magmatism of the granitic rocks from the Ga...

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Published in	Science China. Earth sciences Vol. 52; no. 9; pp. 1240 - 1261
Main Authors	Ji, WeiQiang, Wu, FuYuan, Liu, ChuanZhou, Chung, SunLin
Format	Journal Article
Language	English
Published	Heidelberg SP Science in China Press 01.09.2009 Springer Nature B.V
Subjects	batholith Cretaceous Earth and Environmental Science Earth Sciences Eocene Gangdese Geochemistry geochronology granitic Isotopes Jurassic Lithosphere Magma Mesozoic Miocene Oligocene Paleocene Paleozoic petrogenesis rock Rocks Sediments Tibet granitic rock geochronology Gangdese batholith petrogenesis Tibet
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ISSN	1674-7313 1006-9313 1869-1897 1862-2801
DOI	10.1007/s11430-009-0131-y

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Abstract	Based on petrological and geochemical characteristics such as rock assemblage, petrogeochemistry, Sr-Nd isotope, zircon U-Pb age, and Hf isotope, we studied geochronological framework, magma types, source characters, and petrogenesis of different stages of magmatism of the granitic rocks from the Gangdese batholith in southern Tibet. The magmatic activities of the Gangdese batholith can be divided into three stages. The Mesozoic magmatism, induced by northern subduction of Neotethyan slab, was continuously developed, with two peak periods of Late Jurassic and Early Cretaceous. The Paleocene-Eocene magmatism was the most intensive, and resulted from a complex progress of Neotethyan oceanic slab, including subduction, rollback, and subsequent breakoff. And the Oligocene-Miocene magmatism was attributed to the convective removal of thickened lithosphere in an east-west extension setting after India-Asia collision. Isotopically, zircons from these granitic rocks are characterized by positive εHf(t) values, suggesting that the magmatic source of the Gangdese batholith might be an arc terrane, which was accreted to the southern margin of Asia during Late Paleozoic. Therefore, the chronological framework and Hf isotopic characteristics of the Gangdese batholith are distinct from the granitic rocks in adjacent areas, which can be served as a powerful tracer in studying source-to-sink relation of sediments during the uplift and erosion of Tibetan Plateau.
AbstractList	Based on petrological and geochemical characteristics such as rock assemblage, petrogeochemistry, Sr-Nd isotope, zircon U-Pb age, and Hf isotope, we studied geochronological framework, magma types, source characters, and petrogenesis of different stages of magmatism of the granitic rocks from the Gangdese batholith in southern Tibet. The magmatic activities of the Gangdese batholith can be divided into three stages. The Mesozoic magmatism, induced by northern subduction of Neotethyan slab, was continuously developed, with two peak periods of Late Jurassic and Early Cretaceous. The Paleocene-Eocene magmatism was the most intensive, and resulted from a complex progress of Neotethyan oceanic slab, including subduction, rollback, and subsequent breakoff. And the Oligocene-Miocene magmatism was attributed to the convective removal of thickened lithosphere in an east-west extension setting after India-Asia collision. Isotopically, zircons from these granitic rocks are characterized by positive εHf(t) values, suggesting that the magmatic source of the Gangdese batholith might be an arc terrane, which was accreted to the southern margin of Asia during Late Paleozoic. Therefore, the chronological framework and Hf isotopic characteristics of the Gangdese batholith are distinct from the granitic rocks in adjacent areas, which can be served as a powerful tracer in studying source-to-sink relation of sediments during the uplift and erosion of Tibetan Plateau. Based on petrological and geochemical characteristics such as rock assemblage, petrogeochemistry, Sr-Nd isotope, zircon U-Pb age, and Hf isotope, we studied geochronological framework, magma types, source characters, and petrogenesis of different stages of magmatism of the granitic rocks from the Gangdese batholith in southern Tibet. The magmatic activities of the Gangdese batholith can be divided into three stages. The Mesozoic magmatism, induced by northern subduction of Neotethyan slab, was continuously developed, with two peak periods of Late Jurassic and Early Cretaceous. The Paleocene-Eocene magmatism was the most intensive, and resulted from a complex progress of Neotethyan oceanic slab, including subduction, rollback, and subsequent breakoff. And the Oligocene-Miocene magmatism was attributed to the convective removal of thickened lithosphere in an east-west extension setting after India-Asia collision. Isotopically, zircons from these granitic rocks are characterized by positive ɛ Hf ( t ) values, suggesting that the magmatic source of the Gangdese batholith might be an arc terrane, which was accreted to the southern margin of Asia during Late Paleozoic. Therefore, the chronological framework and Hf isotopic characteristics of the Gangdese batholith are distinct from the granitic rocks in adjacent areas, which can be served as a powerful tracer in studying source-to-sink relation of sediments during the uplift and erosion of Tibetan Plateau. Based on petrological and geochemical characteristics such as rock assemblage, petrogeochemistry, Sr-Nd isotope, zircon U-Pb age, and Hf isotope, we studied geochronological framework, magma types, source characters, and petrogenesis of different stages of magmatism of the granitic rocks from the Gangdese batholith in southern Tibet. The magmatic activities of the Gangdese batholith can be divided into three stages. The Mesozoic magmatism, induced by northern subduction of Neotethyan slab, was continuously developed, with two peak periods of Late Jurassic and Early Cretaceous. The Paleocene-Eocene magmatism was the most intensive, and resulted from a complex progress of Neotethyan oceanic slab, including subduction, rollback, and subsequent breakoff. And the Oligocene-Miocene magmatism was attributed to the convective removal of thickened lithosphere in an east-west extension setting after India-Asia collision. Isotopically, zircons from these granitic rocks are characterized by positive Hf(t) values, suggesting that the magmatic source of the Gangdese batholith might be an arc terrane, which was accreted to the southern margin of Asia during Late Paleozoic. Therefore, the chronological framework and Hf isotopic characteristics of the Gangdese batholith are distinct from the granitic rocks in adjacent areas, which can be served as a powerful tracer in studying source-to-sink relation of sediments during the uplift and erosion of Tibetan Plateau. [PUBLICATION ABSTRACT]
Author	Liu, ChuanZhou Ji, WeiQiang Chung, SunLin Wu, FuYuan
Author_xml	– sequence: 1 givenname: WeiQiang surname: Ji fullname: Ji, WeiQiang organization: State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Graduate University of Chinese Academy of Sciences – sequence: 2 givenname: FuYuan surname: Wu fullname: Wu, FuYuan email: wufuyuan@mail.iggcas.ac.cn organization: State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences – sequence: 3 givenname: ChuanZhou surname: Liu fullname: Liu, ChuanZhou organization: State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences – sequence: 4 givenname: SunLin surname: Chung fullname: Chung, SunLin organization: Department of Geoscience, Taiwan University
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Issue	9
Keywords	granitic rock geochronology Gangdese batholith petrogenesis Tibet
Language	English
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Notes	JI WeiQiang1,2, WU FuYuan1, LIU ChuanZhou1 & CHUNG SunLin3 1 State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China; 2 Graduate University of Chinese Academy of Sciences, Beijing 100049, China; 3 Department of Geoscience, Taiwan University, Taipei 106, China 11-5843/P SourceType-Scholarly Journals-1 ObjectType-Feature-1 content type line 14
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PublicationTitle	Science China. Earth sciences
PublicationTitleAbbrev	Sci. China Ser. D-Earth Sci
PublicationTitleAlternate	SCIENCE CHINA Earth Sciences
PublicationYear	2009
Publisher	SP Science in China Press Springer Nature B.V
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Snippet	Based on petrological and geochemical characteristics such as rock assemblage, petrogeochemistry, Sr-Nd isotope, zircon U-Pb age, and Hf isotope, we studied...
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SubjectTerms	batholith Cretaceous Earth and Environmental Science Earth Sciences Eocene Gangdese Geochemistry geochronology granitic Isotopes Jurassic Lithosphere Magma Mesozoic Miocene Oligocene Paleocene Paleozoic petrogenesis rock Rocks Sediments Tibet
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Title	Geochronology and petrogenesis of granitic rocks in Gangdese batholith, southern Tibet
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