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Article: Unique Carboniferous-Permian tectonic-metallogenic framework of Northern Xinjiang (NW China): Constraints for the tectonics of the southern Paleoasian Domain

TitleUnique Carboniferous-Permian tectonic-metallogenic framework of Northern Xinjiang (NW China): Constraints for the tectonics of the southern Paleoasian Domain
新疆北部石炭纪•二叠纪独特的构造•成矿作用: 对古亚洲洋构造域南部大地构造演化的制约
Authors
Keywords石炭纪一二叠世构造一成矿事件 (Carboniferous-Early Permian Tectonic-Metallogenic Framework)
新疆北部 (North Xinjiang)
古亚洲洋构造域南部 (Southern Paleoasian Domain)
Issue Date2006
PublisherChinese Academy of Sciences, Institute of Geology and Geophysics. The Journal's web site is located at http://www.ysxb.ac.cn/ysxb/ch/index.aspx
Citation
Acta Petrologica Sinica, 2006, v. 22 n. 5, p. 1062-1076 How to Cite?
AbstractThe late Paleozoic tectonic-metallogenic framework of North Xinjiang of the southern Paleoasian Domain was characterized by a serious of Carboniferous-Permian events, including: (1) late Carboniferous-Permian Chinese Altay island arc and its metamorphism, granulite in the Chinese Altay, radiolarian chert and high-pressure/ultra-high-pressure metamorphism; (2) late Carboniferous-early Permian adakites, Alaskan-type mafic-ultramafic complexes, and calc-alkaline magmatism, together with porphyry copper deposits, which occurred in the North Xinjiang; and (3) late Carboniferous ophiolite and island arc volcanic rocks located in the Tian Shan. Combined with the facts that there was no typical foreland basin, no typical collisional-type granitoid, and there were large amount of strike-slip faulting, it is suggested that in the Carboniferous-early Permian North Xinjiang was characterized by the coexistence of compression-extension-strike-slip structures with active magmatism and metallogeny. These phenomena all indicate that there were active margins during the late Carboniferous-early Permian, leading to the notion that the complicated accretionary orogeny along the southern Paleoasian Domain may have lasted to the latest Carboniferous-Permian.
新疆北部晚古生代独特的构造一成矿作用以发育大量石炭纪一二叠纪构造一成矿事件为特征, 其中包括: (l) 发育于晚石炭世一二叠世的阿尔泰岛弧及其变质事件、阿尔泰麻粒岩与基性杂岩、西南天山放射虫硅质岩和高压一超高压一低压麻拉岩相变质事件; (2 )北疆发育的石炭纪(一二叠世)埃达克岩一高镁安山岩一富N d 玄武质岩组合、阿拉斯加型基性一超基性杂岩和大量的与俯冲相关的钙碱性岩浆活动与斑岩型铜矿床成矿作用; (3) 天山晚石炭世晚期蛇绿岩与岛弧火山岩等。结合北疆地区相关的前陆盆地发育不明显、碰撞型花岗岩欠发育与大量发育平行造山带大型走滑构造等现象, 可以认为新疆北部在石炭纪一二叠纪挤压一伸展一走滑并存, 岩浆活动与成矿作用活跃。这些新进展表明新疆北部在晚石炭世一二叠纪可能仍存在活动陆缘, 因此, 古亚洲洋构造域南部复杂增生造山作用最后延至晚石炭世晚期一二叠纪。
Persistent Identifierhttp://hdl.handle.net/10722/151195
ISSN
2015 Impact Factor: 1.234
2015 SCImago Journal Rankings: 0.892
References

 

DC FieldValueLanguage
dc.contributor.authorXiao, WJen_US
dc.contributor.authorHan, CMen_US
dc.contributor.authorYuan, Cen_US
dc.contributor.authorChen, HLen_US
dc.contributor.authorSun, Men_US
dc.contributor.authorLin, SFen_US
dc.contributor.authorLi, ZLen_US
dc.contributor.authorMao, QGen_US
dc.contributor.authorZhang, JEen_US
dc.contributor.authorSun, Sen_US
dc.contributor.authorLi, JLen_US
dc.date.accessioned2012-06-26T06:18:30Z-
dc.date.available2012-06-26T06:18:30Z-
dc.date.issued2006en_US
dc.identifier.citationActa Petrologica Sinica, 2006, v. 22 n. 5, p. 1062-1076en_US
dc.identifier.issn1000-0569en_US
dc.identifier.urihttp://hdl.handle.net/10722/151195-
dc.description.abstractThe late Paleozoic tectonic-metallogenic framework of North Xinjiang of the southern Paleoasian Domain was characterized by a serious of Carboniferous-Permian events, including: (1) late Carboniferous-Permian Chinese Altay island arc and its metamorphism, granulite in the Chinese Altay, radiolarian chert and high-pressure/ultra-high-pressure metamorphism; (2) late Carboniferous-early Permian adakites, Alaskan-type mafic-ultramafic complexes, and calc-alkaline magmatism, together with porphyry copper deposits, which occurred in the North Xinjiang; and (3) late Carboniferous ophiolite and island arc volcanic rocks located in the Tian Shan. Combined with the facts that there was no typical foreland basin, no typical collisional-type granitoid, and there were large amount of strike-slip faulting, it is suggested that in the Carboniferous-early Permian North Xinjiang was characterized by the coexistence of compression-extension-strike-slip structures with active magmatism and metallogeny. These phenomena all indicate that there were active margins during the late Carboniferous-early Permian, leading to the notion that the complicated accretionary orogeny along the southern Paleoasian Domain may have lasted to the latest Carboniferous-Permian.en_US
dc.description.abstract新疆北部晚古生代独特的构造一成矿作用以发育大量石炭纪一二叠纪构造一成矿事件为特征, 其中包括: (l) 发育于晚石炭世一二叠世的阿尔泰岛弧及其变质事件、阿尔泰麻粒岩与基性杂岩、西南天山放射虫硅质岩和高压一超高压一低压麻拉岩相变质事件; (2 )北疆发育的石炭纪(一二叠世)埃达克岩一高镁安山岩一富N d 玄武质岩组合、阿拉斯加型基性一超基性杂岩和大量的与俯冲相关的钙碱性岩浆活动与斑岩型铜矿床成矿作用; (3) 天山晚石炭世晚期蛇绿岩与岛弧火山岩等。结合北疆地区相关的前陆盆地发育不明显、碰撞型花岗岩欠发育与大量发育平行造山带大型走滑构造等现象, 可以认为新疆北部在石炭纪一二叠纪挤压一伸展一走滑并存, 岩浆活动与成矿作用活跃。这些新进展表明新疆北部在晚石炭世一二叠纪可能仍存在活动陆缘, 因此, 古亚洲洋构造域南部复杂增生造山作用最后延至晚石炭世晚期一二叠纪。-
dc.languagechien_US
dc.publisherChinese Academy of Sciences, Institute of Geology and Geophysics. The Journal's web site is located at http://www.ysxb.ac.cn/ysxb/ch/index.aspxen_US
dc.relation.ispartofActa Petrologica Sinicaen_US
dc.relation.ispartof岩石学报-
dc.rightsCreative Commons: Attribution 3.0 Hong Kong License-
dc.subject石炭纪一二叠世构造一成矿事件 (Carboniferous-Early Permian Tectonic-Metallogenic Framework)en_US
dc.subject新疆北部 (North Xinjiang)en_US
dc.subject古亚洲洋构造域南部 (Southern Paleoasian Domain)en_US
dc.titleUnique Carboniferous-Permian tectonic-metallogenic framework of Northern Xinjiang (NW China): Constraints for the tectonics of the southern Paleoasian Domainen_US
dc.title新疆北部石炭纪•二叠纪独特的构造•成矿作用: 对古亚洲洋构造域南部大地构造演化的制约-
dc.typeArticleen_US
dc.identifier.emailSun, M: minsun@hku.hken_US
dc.identifier.authoritySun, M=rp00780en_US
dc.description.naturepublished_or_final_versionen_US
dc.identifier.scopuseid_2-s2.0-33749412653en_US
dc.identifier.hkuros127646-
dc.relation.referenceshttp://www.scopus.com/mlt/select.url?eid=2-s2.0-33749412653&selection=ref&src=s&origin=recordpageen_US
dc.identifier.volume22en_US
dc.identifier.issue5en_US
dc.identifier.spage1062en_US
dc.identifier.epage1076en_US
dc.publisher.placeChinaen_US
dc.identifier.scopusauthoridXiao, WJ=7202456615en_US
dc.identifier.scopusauthoridHan, CM=35794513200en_US
dc.identifier.scopusauthoridYuan, C=35241599200en_US
dc.identifier.scopusauthoridChen, HL=8620950800en_US
dc.identifier.scopusauthoridSun, M=25932315800en_US
dc.identifier.scopusauthoridLin, SF=7407611598en_US
dc.identifier.scopusauthoridLi, ZL=7409073311en_US
dc.identifier.scopusauthoridMao, QG=35916504900en_US
dc.identifier.scopusauthoridZhang, JE=14009581400en_US
dc.identifier.scopusauthoridSun, S=7404509994en_US
dc.identifier.scopusauthoridLi, JL=26643194200en_US

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