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西天山特克斯达坂岩基解体的地球化学证据及钼找矿意义

ISSN号：1000-6524
期刊名称：《岩石矿物学杂志》
时间：0
分类：P588.12[天文地球—岩石学;天文地球—地质学] P618.65[天文地球—矿床学;天文地球—地质学]
作者机构：[1]中国地质大学地球科学与资源学院,北京100083, [2]新疆维吾尔自治区地质矿产勘查开发局,新疆乌鲁木齐830000, [3]长安大学地球科学与资源学院,陕西西安710054
相关基金：基金项目：国家自然科学基金资助项目（40534020）;新疆维吾尔自治区地质矿产调查资助项目（XJQDZ2003-24）

作者：李卫东[1,2], 周继兵[1,2], 李永军[3], 庞振甲[3], 栾新东[2]

关键词：岩基解体, 地球化学, 找矿及构造意义, 特克斯达坂, 西天山, batholith disintegration, geochemistry, ore-prospecting and tectonic significance, Tekesi Daban, West Tianshan Mountain

中文摘要：

西天山特克斯达坂岩基可解体为早石炭世库勒萨依序列和早二叠世其那尔萨依序列。库勒萨依序列为钙碱性岛弧斑岩组合,SiO2含量为57.06%-70.74%,σ值平均〈3.26,（Na2O＋K2O）/Al2O3〈0.9,高Al2O3、Na2O、Sr,相对富集LREE,低MgO、Y、Yb,亏损HREE,Na2O/K2O值大都〉1,Sr/Y平均值57.67,δEu平均1.22,具有典型O型Adakite岩特征,Cu、Mo、W等元素富集,已发现Mo矿体。其那尔萨依序列SiO2含量为76.75%-77.83%,σ值平均4.28,（Na2O＋K2O）/Al2O3〉0.9,δEu平均0.07,相对贫Ba、Sr、Ni、Sc,富Rb、Y、Zr、Th、Ta等,Sr/Y值平均3.24,属正常壳源板内裂谷碱性花岗岩类。地球化学特征不仅为这一岩基的解体提供了有力证据,而且对深化区域成矿规律、丰富构造岩石组合、指导进一步找矿和探讨本区大地构造演化均有重要意义。

英文摘要：

The Tekesi Dahan batholith can be divided into two intrusive series, i.e., Early Carboniferous Kulesayi series and Early Permian Qinaersayi series. The porphyry assemblage of the Kulesayi series is a talc-alkaline series formed in an island arc environment. SiO2 is 57.06%-70.74%, the Rittmann index （σ） is lower than 3.26, and （Na2O ＋ K2O）/AlaO3 is lower than 0.9. It is enriched in Al2O3, Na2O, Sr and LREE, and poor in MgO, Y, Yb and HREE; Na2O/K2O is higher than 1, Sr/Y is 57.67, δEu is 1.22, indicating O-type adakite. The Kulesayi series is enriched in Cu, Mo and W, and even contains Mo ore bodies. In the Qinaersayi series, SiO2 is 76.75 %-77.83 %, σ is higher than 3.3, （Na2O ＋ K2O）/Al2O3 is higher than 0.9, and δEu is 0.07 ; this series is poor in Ba, Sr, Ni, Sc but enriched in Rb, Y, Zr, Th, Ta, with Sr/Y being 3.24. The protolith was partly derived from melting of argillaceous rocks of the earth crust, belonging to the alkaline series formed in an intraplate rift environment. Geochemical characteristics provide not only powerful evidence for the disintegration of the Tekesi Dahan batholith but also abundant information for the improvement of native metallogenic regularity. In addition, these characteristics enrich types of tectonite assemblage, guide oreprospecting work and contribute to researches on tectonic evolution.

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