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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:

第44卷

期数:

2022年第03期

页码:

466-480

栏目:

基础地质与矿产地质

出版日期:

2022-05-15

文章信息/Info

Title:

Petrogenesis of Early Carboniferous High-Mg Andesite and Its Tectonic Significance in the Southern Tectonic Belt of Yining Block, China

文章编号:

1672-6561(2022)03-0466-15

作者:

王祚鹏¹; 李永军²; 杨高学²; 李甘雨³; 李 海⁴

(1. 长安大学 地质工程与测绘学院,陕西 西安 710054; 2. 长安大学 地球科学与资源学院,陕西 西安 710054; 3. 河北地质大学 教学发展中心,河北 石家庄 050031; 4. 西安石油大学 地球科学与工程学院,陕西 西安 710065)

Author(s):

WANG Zuo-peng¹;  LI Yong-jun²;  YANG Gao-xue²;  LI Gan-yu³;  LI Hai⁴

(1. School of Geological Engineering and Geomatics, Chang'an University, Xi'an 710054, Shaanxi, China; 2. School of Earth Science and Resources, Chang'an University, Xi'an 710054, Shaanxi, China; 3. Teaching Development Center, Hebei GEO University, Shijiazhuang 050031, Hebei, China; 4. School of Earth Sciences and Engineering, Xi'an Shiyou University, Xi'an 710065, Shaanxi, China)

关键词:

高镁安山岩;  地球化学;  岩石成因;  构造演化;  大哈拉军山组;  早石炭世;  南天山洋;  伊宁地块

Keywords:

high-Mg andesite;  geochemistry;  petrogenesis;  tectonic setting;  Dahalajunshan Formation;  Early Carboniferous;  South Tianshan ocean;  Yining block

分类号:

P588.12; P595

DOI:

10.19814/j.jese.2022.01027

文献标志码:

A

摘要:

伊宁地块南构造带出露大面积的晚泥盆世—早石炭世岩浆岩,其形成与南天山洋演化密切相关,在岩石成因与产出环境方面尚存争议。在伊宁地块南构造带科克苏林场一带新发现了赋存于下石炭统大哈拉军山组火山岩中的高镁安山岩,对其进行了详细的野外地质调查和室内分析工作,并探讨了该时期的大地构造背景。结果表明:区内大哈拉军山组岩石类型以安山岩类为主,含少量玄武岩及火山碎屑岩; 安山岩样品具有高的MgO、TiO₂、Al₂O₃含量和低的P₂O₅含量、里特曼指数,表现出中—高钾钙碱性系列岩石特征,结合其高的Sr、Y含量和低的Ni、Co含量,低的Sr/Y、La/Yb值,呈现出赞岐质高镁安山岩的地球化学特征; 样品的稀土元素总含量变化范围大,具有高的(La/Yb)_N、(La/Sm)_N和(Gd/Yb)_N值,显示出轻稀土元素显著富集特征; 样品富集K、Ba、Th、U、Pb等大离子亲石元素,相对亏损Nb、Ta、Ti、P等高场强元素和负的Eu异常。结合区域资料认为,这些赞岐质高镁安山岩源于地幔楔和俯冲带物质的平衡反应,是晚泥盆世—早石炭世南天山洋在伊宁地块南构造带之下向北俯冲的产物。高镁安山岩的发现不仅丰富了该地区的岩石类型,而且对解决区域构造演化问题提供了重要参考。

Abstract:

A large volume of Late Devonian-Early Carboniferous magmatic rocks are exposed in the southern tectonic belt of Yining block, and their formation is closely related to the evolution of South Tianshan ocean. However, the petrogenesis and tectonic setting of these rocks remain poorly understood. High-Mg andesite in the volcanic rocks of Lower Carboniferous Dahalajunshan Formation in Kekesu Linchang area, the southern tectonic belt of Yining block was discovered. Detailed field geological survey and indoor analysis were carried out for the high-Mg andesite, and the tectonic setting during this period was discussed. The rock types of Dahalajunshan Formation in the research area are dominated by andesites with minor of basalts and pyroclastic rocks. Whole-rock major elements show that the high-Mg andesite samples are characterized by high SiO₂, TiO₂, Al₂O₃, and MgO, coupled with low P₂O₅ and Rittman index, displaying the features of medium-high potassium calc-alkaline series rocks; the contents of REE in these samples vary widely with high(La/Yb)_N,(La/Sm)_N and(Gd/Yb)_N values, showing significant enrichment of LREE. Additionally, it is enriched in LILE, such as K, Ba, Th, U, and Pb, but relatively depleted in HFSE including Nb, Ta, Ti, and P, as well as negative Eu anomaly. Meanwhile, the samples contain high Sr and Y contents, and low Ni content, with low Sr/Y and La/Yb values, which are similar to the geochemical characteristics of sanukitic high-Mg andesite. Combined with regional data, it is argued that the sanukitic high-Mg andesite in the research area originates from the equilibrium reaction between the mantle wedge and the subduction zone materials, which may result from the subduction of South Tianshan ocean under the southern tectonic belt of Yining block from Late Devonian to Early Carboniferous. The discovery of high-Mg andesite not only enriches the rock types in this area, but also provides an important reference for solving the controversy on regional tectonic evolution.

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备注/Memo

备注/Memo:

收稿日期:2022-01-21; 修回日期:2022-03-20
基金项目:国家自然科学基金项目(41672285); 中央高校基本科研业务费专项资金项目(300102271403)
作者简介:王祚鹏(1990-),男,甘肃会宁人,理学博士,博士后,E-mail:zpwang@chd.edu.cn。

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更新日期/Last Update: 2022-06-01