必须声明标量变量 "@Script_ID"。 伊犁地块北缘别珍套山中泥盆统汗吉尕组物源特征及其地质意义-《地球科学与环境学报》
|本期目录/Table of Contents|

[1]陈有炘,裴先治*,王 盟,等.伊犁地块北缘别珍套山中泥盆统汗吉尕组物源特征及其地质意义[J].地球科学与环境学报,2021,43(03):469-486.[doi:10.19814/j.jese.2021.01029]
 CHEN You-xin,PEI Xian-zhi*,WANG Meng,et al.Provenance Characteristics and Geological Significance of the Middle Devonian Hanjiga Formation in Biezhentao Mountain, the Northern Margin of Yili Block, China[J].Journal of Earth Sciences and Environment,2021,43(03):469-486.[doi:10.19814/j.jese.2021.01029]





Provenance Characteristics and Geological Significance of the Middle Devonian Hanjiga Formation in Biezhentao Mountain, the Northern Margin of Yili Block, China
陈有炘12裴先治12*王 盟12赵 军3布龙巴特3关力伟3朱永胜3刘 雷3
(1. 长安大学 地球科学与资源学院,陕西 西安 710054; 2. 长安大学 西部矿产资源与地质工程教育部重点实验室,陕西 西安 710054; 3. 中国地质调查局乌鲁木齐自然资源综合调查中心,新疆 乌鲁木齐 830057)
CHEN You-xin12 PEI Xian-zhi12* WANG Meng12 ZHAO Jun3 BULONG Ba-te3 GUAN Li-wei3 ZHU Yong-sheng3 LIU Lei3
(1. School of Earth Science and Resources, Chang'an University, Xi'an 710054, Shaanxi, China; 2. Key Laboratory of Western China's Mineral Resources and Geological Engineering of Ministry of Education, Chang'an University, Xi'an 710054, Shaanxi, China; 3. Center of Urumqi Natural Resources Comprehensive Survey, China Geological Survey, Urumqi 830057, Xinjiang, China)
物源特征 微量元素 碎屑锆石U-Pb年龄 中泥盆统 汗吉尕组 伊犁地块 中亚造山带
provenance characteristic trace element detrital zircon U-Pb age Middle Devonian Hanjiga Formation Yili block CAOB
天山造山带位于中亚造山带西南缘,是探索中亚造山带增生造山过程的重要窗口。西北天山是伊犁地块与准噶尔地块的结合部位,保存了两者之间构造演化的重要地质信息。出露于伊犁地块北缘别珍套山的泥盆系是记录西北天山晚古生代早期构造演化过程的重要载体。基于此,对中泥盆统汗吉尕组砂岩进行岩相学和LA-ICP-MS碎屑锆石U-Pb定年与微量元素研究。结果表明:碎屑锆石U-Pb年龄介于500~370 Ma,并可以分为两期,主峰年龄为386 Ma,次峰年龄为490 Ma,结合岩相学和锆石微量元素特征,汗吉尕组砂岩的物源主要为晚古生代早期中酸性岩浆岩和早古生代早—中期中基性岩浆岩。综合分析认为,汗吉尕组于中泥盆世晚期沉积于弧前盆地沉积构造环境,物源主要为伊犁地块北缘的古生代岩浆弧,暗示伊犁地块北缘在晚古生代早期受准噶尔洋向南俯冲作用影响,为活动大陆边缘。
Tianshan orogen, which is located in the southwestern part of the Central Asian orogenic belt(CAOB), is a window to explore the accretionary orogenic process of the CAOB. The northwest Tianshan orogen, which is the joint of Yili block and Junggar block, preserves the important geological information of the evolution between them. Especially, the Devonian exposed in Biezhentao Mountain on the northern margin of Yili block is an important carrier for recording the evolution of the northwest Tianshan in the early Late Paleozoic. Detrital zircon LA-ICP-MS U-Pb dating of sandstone from Hanjiga Formation shows that the ages of detrital zircons range from 500 Ma to 370 Ma, and can be divided into two periods: the main period peak value is 386 Ma, followed by 490 Ma. According to the petrographic characteristics, ages and trace elements of zircon, the provenance of sandstone is mainly intermediate-acid magmatic rock of the early Late Paleozoic and intermediate-basic magmatic rock of the early-middle Early Paleozoic. It is inferred that the sedimentary age of Hanjiga Formation is late Middle Devonian and formed in the forearc basin environment. It is also indicated that the detrital materials of the studied sandstone are mainly derived from the Paleozoic magmatic arc in the northern margin of Yili block, which belongs to the near-source sediments. Meanwhile, it is suggested that the northern margin of Yili block is an active continental margin due to the southward subduction of Junggar ocean in the early Late Paleozoic.


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收稿日期:2021-01-26; 修回日期:2021-03-10
基金项目:国家自然科学基金项目(41802234,42072267); 陕西省自然科学基础研究计划项目(2019JQ-209,2019JQ-090); 中央高校基本科研业务费专项资金项目(300102271207,300102279104,300102279201); 中国地质调查局地质调查项目(12120115041301)
更新日期/Last Update: 2021-05-01