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Early Paleozoic high-temperature metamorphism of garnet amphibolite in the Longyou area, Cathaysia Block of South China: P & ndash;T path and tectonic implications
Qian, Jiahui1,2; Yin, Changqing1,2; Zhang, Jian1,2; Jin, Xin3
2021-06-15
发表期刊JOURNAL OF ASIAN EARTH SCIENCES
ISSN1367-9120
卷号213页码:16
通讯作者Qian, Jiahui([email protected])
摘要Garnet amphibolite can provide crucial information on tectonic processes. Recent progresses on garnet amphibolite in the Longyou area of the Cathaysia Block, South China have attracted geologists? wide concerns and discussions about the regional metamorphic history and geodynamic setting. The Longyou garnet amphibolite shows a prominent porphyroblastic texture involving garnet (-40 vol%), hornblende, clinopyroxene, quartz and ilmenite, with minor plagioclase (<5 vol%), sphene, rutile, pyrite and apatite. Garnet presents as aggregations with double-/multi-nuclear structure and has embayed rims surrounded by quartz and plagioclase. Clinopyroxene is partially replaced by late hornblende and plagioclase. A clockwise high-temperature P?T evolution involving four stages has been determined. The generalized prograde stage shows increases of P?T conditions. The Pmax and Tmax stages lie in P?T conditions of 13 ? 0.6 kbar/808 ? 13 ?C and 10 ? 0.9 kbar/840 ? 10 ?C, reflecting apparent thermal gradients of -17 ?C/km and 22?23 ?C/km, respectively. Both stages match medium-pressure facies series metamorphism. The late retrograde stage shows decompression and cooling. A P?XMg [=Mg/(Mg + Fe) in mole] pseudosection drawn at T = 840 ?C suggests that low bulk-rock XMg contents (=0.29?0.33) in the Longyou garnet amphibolite are responsible for the high content of garnet in the rock. A P?M (Na2O) pseudosection at T = 840 ?C reveals that the low content of plagioclase in the rock is caused by low bulkrock Na2O contents (=0.44?1.18 mol.%). The integrated P?T?t data from the Cathaysia Block indicate that the early Paleozoic metamorphism can be connected to an intraplate orogenic setting.
关键词Garnet amphibolite Phase modeling High-temperature metamorphism Cathaysia Block South China
DOI10.1016/j.jseaes.2021.104744
收录类别SCI
语种英语
资助项目Fundamental Research Funds for the Central Universities[18lgpy17]; Guangdong Basic and Applied Basic Research Foundation[2019A1515012189]; National Natural Science Foundation of China[41972197]
WOS研究方向Geology
WOS类目Geosciences, Multidisciplinary
WOS记录号WOS:000647448700002
出版者PERGAMON-ELSEVIER SCIENCE LTD
引用统计
被引频次:9[WOS]   [WOS记录]     [WOS相关记录]
文献类型期刊论文
条目标识符http://ir.qdio.ac.cn/handle/337002/176772
专题深海极端环境与生命过程研究中心
通讯作者Qian, Jiahui
作者单位1.Sun Yat Sen Univ, Sch Earth Sci & Engn, Guangdong Prov Key Lab Mineral Resources & Geol P, Guangzhou 510275, Guangdong, Peoples R China
2.Southern Marine Sci & Engn Guangdong Lab Zhuhai, Zhuhai, Peoples R China
3.Chinese Acad Sci, Ctr Deep Sea Res, Inst Oceanog, Qingdao 266071, Peoples R China
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Qian, Jiahui,Yin, Changqing,Zhang, Jian,et al. Early Paleozoic high-temperature metamorphism of garnet amphibolite in the Longyou area, Cathaysia Block of South China: P & ndash;T path and tectonic implications[J]. JOURNAL OF ASIAN EARTH SCIENCES,2021,213:16.
APA Qian, Jiahui,Yin, Changqing,Zhang, Jian,&Jin, Xin.(2021).Early Paleozoic high-temperature metamorphism of garnet amphibolite in the Longyou area, Cathaysia Block of South China: P & ndash;T path and tectonic implications.JOURNAL OF ASIAN EARTH SCIENCES,213,16.
MLA Qian, Jiahui,et al."Early Paleozoic high-temperature metamorphism of garnet amphibolite in the Longyou area, Cathaysia Block of South China: P & ndash;T path and tectonic implications".JOURNAL OF ASIAN EARTH SCIENCES 213(2021):16.
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