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

肖文交 韩春明 袁超 陈汉林 孙敏 林寿发 厉子龙 毛启贵 张继恩 孙枢 李继亮. 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[J]. 岩石学报, 2006, 22(5): 1062-1076.
引用本文: 肖文交 韩春明 袁超 陈汉林 孙敏 林寿发 厉子龙 毛启贵 张继恩 孙枢 李继亮. 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[J]. 岩石学报, 2006, 22(5): 1062-1076.
XIAO WenJiao , HAN ChunMing, YUAN Chao, CHEN HanLin, SUN Min, LIN ShouFa, LI ZiLong, MAO QiGui, ZHANG JiEn, SUN Shu and LI JiLiang. Unique Carboniferous-Permian tectonic-metallogenic framework of Northern Xinjiang(NW China):Constraints for the tectonics of the southern Paleoasian Domain.[J]. Acta Petrologica Sinica, 2006, 22(5): 1062-1076.
Citation: XIAO WenJiao , HAN ChunMing, YUAN Chao, CHEN HanLin, SUN Min, LIN ShouFa, LI ZiLong, MAO QiGui, ZHANG JiEn, SUN Shu and LI JiLiang. Unique Carboniferous-Permian tectonic-metallogenic framework of Northern Xinjiang(NW China):Constraints for the tectonics of the southern Paleoasian Domain.[J]. Acta Petrologica Sinica, 2006, 22(5): 1062-1076.

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

  • 基金项目:

    国家重点基础研究发展规划项目(2001CB409801)、国家重点攻关项目(96-915-07)与香港研究基金项目(HKU7140/04P、HKU7058/04P和HKU7055/05P)联合资助.致谢 涂光炽院士、肖序常院士与何国琦教授对本研究工作进行了指导.赵振华研究员、胡霭琴研究员、于学元研究员、王京彬研究员、高俊研究员、秦克章研究员、韩宝福教授、郭召杰博士、刘伟研究员、马瑞士教授以及“中国西部中亚型造山与成矿”项目全体科研人员与作者进行了讨论.李锦轶研究员、徐新教授、周鼎武教授、秦克章研究员、王志

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

  • 新疆北部晚古生代独特的构造-成矿作用以发育大量石炭纪-二叠纪构造-成矿事件为特征,其中包括:(1)发育于晚石炭世-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-超高压-低压麻粒岩相变质事件;(2)北疆发育的石炭纪(-二叠世)埃达克岩-高镁安山岩-富Nd玄武质岩组合、阿拉斯加型基性-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-二叠纪挤压-伸展-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-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-二叠纪。
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出版历程
收稿日期:  2005-12-20
修回日期:  2006-04-10
刊出日期:  2006-05-31

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