Petrogenesis of the Microgranular Enclaves and Their Host Granites from the Xitian Intrusion in South China: Implications for Geodynamic Setting and Mineralization

The South China Block had experienced a significant tectonic transition during the Mesozoic in response to the subduction of the Paleo- and the Pacific Ocean. Large-scale granitic intrusions with massive mineralization are widespread in South China, and their tectonic settings are not defined. The X...
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Autor*in:	Miao He [verfasserIn] Qing Liu [verfasserIn] Quanlin Hou [verfasserIn] Jinfeng Sun [verfasserIn] Quanren Yan [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2020

Schlagwörter:	microgranular enclaves zircon geochronology Hf-O isotopes South China

Übergeordnetes Werk:	In: Minerals - MDPI AG, 2012, 10(2020), 12, p 1059
Übergeordnetes Werk:	volume:10 ; year:2020 ; number:12, p 1059

Links:	Link aufrufen Link aufrufen Link aufrufen Journal toc

DOI / URN:	10.3390/min10121059

Katalog-ID:	DOAJ067044077

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language	English
source	In Minerals 10(2020), 12, p 1059 volume:10 year:2020 number:12, p 1059
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topic_facet	microgranular enclaves zircon geochronology Hf-O isotopes South China Mineralogy
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authorswithroles_txt_mv	Miao He @@aut@@ Qing Liu @@aut@@ Quanlin Hou @@aut@@ Jinfeng Sun @@aut@@ Quanren Yan @@aut@@
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callnumber-first	Q - Science
author	Miao He
spellingShingle	Miao He misc QE351-399.2 misc microgranular enclaves misc zircon geochronology misc Hf-O isotopes misc South China misc Mineralogy Petrogenesis of the Microgranular Enclaves and Their Host Granites from the Xitian Intrusion in South China: Implications for Geodynamic Setting and Mineralization
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topic_title	QE351-399.2 Petrogenesis of the Microgranular Enclaves and Their Host Granites from the Xitian Intrusion in South China: Implications for Geodynamic Setting and Mineralization microgranular enclaves zircon geochronology Hf-O isotopes South China
topic	misc QE351-399.2 misc microgranular enclaves misc zircon geochronology misc Hf-O isotopes misc South China misc Mineralogy
topic_unstemmed	misc QE351-399.2 misc microgranular enclaves misc zircon geochronology misc Hf-O isotopes misc South China misc Mineralogy
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title	Petrogenesis of the Microgranular Enclaves and Their Host Granites from the Xitian Intrusion in South China: Implications for Geodynamic Setting and Mineralization
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title_full	Petrogenesis of the Microgranular Enclaves and Their Host Granites from the Xitian Intrusion in South China: Implications for Geodynamic Setting and Mineralization
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author_browse	Miao He Qing Liu Quanlin Hou Jinfeng Sun Quanren Yan
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title_sort	petrogenesis of the microgranular enclaves and their host granites from the xitian intrusion in south china: implications for geodynamic setting and mineralization
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title_auth	Petrogenesis of the Microgranular Enclaves and Their Host Granites from the Xitian Intrusion in South China: Implications for Geodynamic Setting and Mineralization
abstract	The South China Block had experienced a significant tectonic transition during the Mesozoic in response to the subduction of the Paleo- and the Pacific Ocean. Large-scale granitic intrusions with massive mineralization are widespread in South China, and their tectonic settings are not defined. The Xitian intrusion is ideal for probing the geodynamic setting and mineralization in South China because they comprise an abundance of microgranular enclaves (MEs) and diverse types of granite associated with mineralization. Age determined by zircon U-Pb dating suggests that the MEs and their host granites are coeval within error, of ca. 152 Ma. The MEs have a similar initial Hf-O isotopic composition as host granites, and the rapid cooling mineral textures indicate that they are autoliths. Geochemical data show that the host granites are high-K, calc-alkaline, and transitional from metaluminous to peraluminous, slightly enriched in light rare earth elements (LREEs) relative to heavy rare earth elements (HREEs), with obvious negative Eu anomalies, belonging to I-type. The Nb/Ta and Zr/Hf ratios indicate the volatile penetrates the magmatic-forming process, and the fluid with abundant volatile could extract metal element effectively from the mantle.
abstractGer	The South China Block had experienced a significant tectonic transition during the Mesozoic in response to the subduction of the Paleo- and the Pacific Ocean. Large-scale granitic intrusions with massive mineralization are widespread in South China, and their tectonic settings are not defined. The Xitian intrusion is ideal for probing the geodynamic setting and mineralization in South China because they comprise an abundance of microgranular enclaves (MEs) and diverse types of granite associated with mineralization. Age determined by zircon U-Pb dating suggests that the MEs and their host granites are coeval within error, of ca. 152 Ma. The MEs have a similar initial Hf-O isotopic composition as host granites, and the rapid cooling mineral textures indicate that they are autoliths. Geochemical data show that the host granites are high-K, calc-alkaline, and transitional from metaluminous to peraluminous, slightly enriched in light rare earth elements (LREEs) relative to heavy rare earth elements (HREEs), with obvious negative Eu anomalies, belonging to I-type. The Nb/Ta and Zr/Hf ratios indicate the volatile penetrates the magmatic-forming process, and the fluid with abundant volatile could extract metal element effectively from the mantle.
abstract_unstemmed	The South China Block had experienced a significant tectonic transition during the Mesozoic in response to the subduction of the Paleo- and the Pacific Ocean. Large-scale granitic intrusions with massive mineralization are widespread in South China, and their tectonic settings are not defined. The Xitian intrusion is ideal for probing the geodynamic setting and mineralization in South China because they comprise an abundance of microgranular enclaves (MEs) and diverse types of granite associated with mineralization. Age determined by zircon U-Pb dating suggests that the MEs and their host granites are coeval within error, of ca. 152 Ma. The MEs have a similar initial Hf-O isotopic composition as host granites, and the rapid cooling mineral textures indicate that they are autoliths. Geochemical data show that the host granites are high-K, calc-alkaline, and transitional from metaluminous to peraluminous, slightly enriched in light rare earth elements (LREEs) relative to heavy rare earth elements (HREEs), with obvious negative Eu anomalies, belonging to I-type. The Nb/Ta and Zr/Hf ratios indicate the volatile penetrates the magmatic-forming process, and the fluid with abundant volatile could extract metal element effectively from the mantle.
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title_short	Petrogenesis of the Microgranular Enclaves and Their Host Granites from the Xitian Intrusion in South China: Implications for Geodynamic Setting and Mineralization
url	https://doi.org/10.3390/min10121059 https://doaj.org/article/e13647cb991c4b358b4e2aea8834ad2b https://www.mdpi.com/2075-163X/10/12/1059 https://doaj.org/toc/2075-163X
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up_date	2024-07-03T23:17:01.764Z
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Petrogenesis of the Microgranular Enclaves and Their Host Granites from the Xitian Intrusion in South China: Implications for Geodynamic Setting and Mineralization

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