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西天山那拉提构造带及邻区几个地层问题的讨论
引用本文:杨志华,王宏君,邓亚婷,倪新源,何建喜,李兵,胡志军,宋俊峰,周晓飞,李红兵.西天山那拉提构造带及邻区几个地层问题的讨论[J].陕西地质,2006,24(1):12-26.
作者姓名:杨志华  王宏君  邓亚婷  倪新源  何建喜  李兵  胡志军  宋俊峰  周晓飞  李红兵
作者单位:1. 长安大学地球科学学院及国土资源部成矿作用及其动力学开放研究实验室,西安,710054
2. 新疆地质调查院,乌鲁木齐,830000
3. 陕西省国土资源信息中心,西安,710054
4. 新疆地质调查院第四地质调查所,昌吉,831100
基金项目:新疆地质调查院基金;新疆地质调查院基金;新疆地质调查院基金;新疆地质调查院基金;新疆地质调查院基金;新疆地质调查院基金;新疆地质调查院基金;新疆地质调查院基金;新疆地质调查院基金;新疆地质调查院基金
摘    要:西天山—伊宁地区以独特的结构特征和关键的大地构造部位,历来成为中外地质学家所关注、研究的重要地区,而那拉提构造带及邻区又在西天山—伊宁地区占有举足轻重的地位。由于客观条件的制约,那拉提构造带及西天山造山带在基础地质的许多方面存在不少问题,直接影响到对天山造山带和伊犁盆地的正确认识。笔者根据近十年来在那拉提带及邻区进行10个1∶5万区调填图和收集到的其它资料,对该区几个重要层位的时代、大哈拉军山火山岩系的形成背景、蛇绿岩和蓝闪片岩的产出特征以及该区的结构、构造单元划分和发展演化的动力学机制进行了讨论,其中的许多认识和看法将对该区的进一步研究产生推动作用。

关 键 词:那拉提构造带  地层时代  蛇绿岩和蓝闪片岩  大哈拉军山火山岩系形成背景  结构特征  中国新疆
文章编号:1001-6996(2006)01-0012-15
收稿时间:2005-10-12
修稿时间:2005年10月12

DISCUSSION ABOUT SEVERAL GEOLOGIC QUESTIONS IN NALAQI STRCTURE BELT AND ITS ADJACENT REGIONS,WEST TIANSHAN MT
YANG Zhi-hua, WANG Hong-jun, SU Chun-qin, LI Yong, QI NI Xin-yuan, HE Jian-xi, LI Bin, DANG Ya-ting, Shi-jun, GUO Jun-feng.DISCUSSION ABOUT SEVERAL GEOLOGIC QUESTIONS IN NALAQI STRCTURE BELT AND ITS ADJACENT REGIONS,WEST TIANSHAN MT[J].Geology of Shaanxi,2006,24(1):12-26.
Authors:YANG Zhi-hua  WANG Hong-jun  SU Chun-qin  LI Yong  QI NI Xin-yuan  HE Jian-xi  LI Bin  DANG Ya-ting  Shi-jun  GUO Jun-feng
Abstract:The area of West Tianshan-Yining,with its special geology and key tectonic characteristics,has been a fascinated place for domestic and foreign geologists.Nalaqi structure belt and its neighbor region are very important to the geology study in the area of West Tianshan-Yining.There are many questions about several aspects of the basic geology in Nalaqi structure belt and West Tianshan Orogen,of which directly influence understanding to the geology of Tianshan orogen and Yining Basin.In this paper,on the basis of the document got in last ten years from the regional geology surveying and mapping with the scale of 1:50000 as well as other geology materials,the author systematic discusses the geology problems,including the time of the main strata,the background of the formation of Dahala Junshan volcanic rock,occurrence of the ophiolite and glaucophane schist,the division of the structure and tectonic elements and its development evolution,in the Nalaqi structure belt and its neighbor region.Knownledg and ideas of this paper are vey useful and would be promote further study to the geology in the area.
Keywords:Nalaqi structure belt  the time of the main strata  the ophiolite and glaucophane schist  the background of the formation of Dahala Junshan volcanic rock  characteristics of the texture  Xinjiang China
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