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新疆西天山大哈拉军山组火山岩岩石化学特征及地质意义
引用本文:邵铁全,石莹,靳红,宋杨,朱志新,王克卓,张建东,徐达.新疆西天山大哈拉军山组火山岩岩石化学特征及地质意义[J].新疆地质,2006,24(3):218-222.
作者姓名:邵铁全  石莹  靳红  宋杨  朱志新  王克卓  张建东  徐达
作者单位:1. 长安大学地质工程与测绘工程学院,陕西,西安,710054
2. 新疆维吾尔自治区地质矿产勘查开发局第一区域地质调查大队,新疆,乌鲁木齐,830011
3. 新疆维吾尔自治区地质矿产研究所,新疆,乌鲁木齐,830000
4. 中国地质大学,北京,10083
5. 新疆维吾尔自治区地质矿产勘查开发局第一区域地质调查大队,新疆,乌鲁木齐,830011;中国地质科学院地质研究所,北京,100037
基金项目:中国地调局大调查项目(200213000018)资助
摘    要:下石炭统大哈拉军山组主要分布于西天山伊犁盆地,不整合在志留纪地层或老地层之上,其上被阿克萨克组角度或平行不整合覆盖.火山岩组合为玄武岩、安山岩、流纹岩及安山岩、流纹岩组合,以安山岩发育为特征.玄武岩属岛弧拉斑玄武岩和钙碱性系列,属太平洋型钠质类型,稀土、微量元素显示具岛弧特征,大地构造位置为岛弧中心靠近大洋一侧,与南侧那拉提晚泥盆—早石炭世侵入岩共同组成火山弧,同为古亚洲洋向北俯冲的产物.

关 键 词:西天山  大哈拉军山组  火山岩  岛弧
文章编号:1000-8845(2006)03-218-05
收稿时间:09 23 2005 12:00AM
修稿时间:01 16 2006 12:00AM

VOLCANIC ROCK PETROCHEMICAL CHARACTERISTICS OF THE DAIHALAJUNSHAN FORMATION IN THE WESTERN TIANSHAN, XINJIANG AND THEIR GEOLOGICAL SIGNIFICANCE
SHAO Tie-quan, SHI Ying, JIN Hong, SONG Yang, ZHU Zhi-xin, WANG Ke-zhuo, ZHAN Jian-dong, XU Da.VOLCANIC ROCK PETROCHEMICAL CHARACTERISTICS OF THE DAIHALAJUNSHAN FORMATION IN THE WESTERN TIANSHAN, XINJIANG AND THEIR GEOLOGICAL SIGNIFICANCE[J].Xinjiang Geology,2006,24(3):218-222.
Authors:SHAO Tie-quan  SHI Ying  JIN Hong  SONG Yang  ZHU Zhi-xin  WANG Ke-zhuo  ZHAN Jian-dong  XU Da
Abstract:daihalajunshan formation of early carboniferous was been mostly distributed in yili basin of western tianshan, it unconformity cover on the Silurian stratum and older stratum,and was been covered by akesake formation in angular unconformity and disconformity. the volcanic rock combination is basalt-andesite-rhyolite and andesite-rhyolite. the basalt is belong island arc tholeiite and series of the calc-alkaline,and have character of island arc in rare earth element and trace element. The tectonic location at the center of island arc and close up ocean. It consist volcanic arc together with the plutons of lanati in the late Devonian-early carboniferous. the volcanic arc was the result of ancient asia ocean subduct northward.
Keywords:western tianshan  daihalajunshan formation  volcanic rock  island arc
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