东天山晚古生代构造转折红山南|8、沉积岩与岩浆岩的接触关系_褶皱构造

东天山晚古生代构造转折: 红山南-天木东地区岩浆岩年代学与地球化学的约束

中国科学院新疆生态与地理研究所, 荒漠与绿洲生态国家重点实验室, 乌鲁木齐 830011

新疆矿产资源与数字地质实验室, 乌鲁木齐 830011

中国科学院新疆矿产资源研究中心, 乌鲁木齐 830011

中国科学院大学, 北京 100049

长安大学地球科学与资源学院, 西安 710054

北京大学, 造山带与地壳演化教育部重点实验室, 北京 100871

本文受国家自然科学基金项目(42072106)、新疆自治区自然科学基金项目(2022D01A344)及长安大学中央高校基本科研业务费专项资金领军人才项目(300102271302)联合资助

中图分类号:P588.1;P597.3

State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China

Xinjiang Key Laboratory of Mineral Resources and Digital Geology, Urumqi 830011, China

Xinjiang Research Centre for Mineral Resources, Chinese Academy of Sciences, Urumqi 830011, China

University of Chinese Academy of Sciences, Beijing 100049, China

School of Earth Science and Resources, Chang'an University, Xi'an 710054, China

MOE Key Laboratory of Orogenic Belts and Crustal Evolution, Peking University, Beijing 100871, China

东天山是中亚造山带的重要组成部分, 区内晚古生代岩浆活动与成矿作用强烈, 是理解中亚造山带构造演化与成矿作用的关键地区。然而, 前人对东天山构造带由俯冲向碰撞转变的时间和过程仍存在较大争议。本文对东天山红山南-天木东地区广泛出露的晚古生代岩浆岩开展了野外考察和岩相学鉴定, 进行了年代学和岩石地球化学分析, 以限定其形成时代、岩石成因和构造背景, 进而探讨晚古生代构造演化过程。红山南-天木东地区岩浆岩主要为早石炭世火山岩和侵入岩, 次为早二叠世侵入岩。早石炭世火山岩主要为安山岩(328.8±2.0Ma)和英安岩, 侵入岩主要为辉长闪长岩(328.7±1.8Ma); 早二叠世侵入岩为黑云母二长花岗岩(290.3±2.1Ma)和石英闪长岩(290.0±1.6Ma)。早石炭世岩浆岩富含角闪石和斜长石, 为钙碱性, 准铝质系列, 富Rb、Ba、Th、U和Pb等大离子亲石元素, 亏损Nb、Ta和Ti等高场强元素和Sr-Nd-Hf同位素, 具有岛弧岩浆岩特征, 是交代地幔楔部分熔融的产物。相对于早石炭世岩浆岩, 早二叠世侵入岩富含黑云母和碱性长石, 富集SiO2、Na2O和K2O, 贫Al2O3、MgO、Fe2O3T及CaO, 同位素更亏损, 为碰撞后背景下新生加厚地壳部分熔融的产物。总之, 红山南-天木东地区的早石炭世与早二叠世岩浆岩地球化学差异显著, 指示东天山构造背景从早石炭世大洋俯冲体制转变为早二叠世碰撞后造山体制, 即其构造转折时间为晚石炭世-早二叠世。

The East Tianshan, as an important part of the Central Asian Orogenic Belt (CAOB), is characterized by its extensive Late Paleozoic magmatism and metallogeny, and thus serves as a critical area for understanding the tectonic evolution and metallogeny of the southern CAOB. Nevertheless, the time and process of tectonic transition from subduction to collision of the East Tianshan remain debate. In this contribution, detailed field investigation, petrographic observation, geochronological and geochemical analysis have been conducted to constrain the ages, genesis and tectonic settings of the Late Paleozoic igneous rocks in the Hongshannan-Tianmudong area. Petrological and zircon U-Pb dating results indicate that the Early Carboniferous volcanic rocks are mainly composed of andesite (328.8±2.0Ma) and dacite, while the intrusive rocks are gabbro-diorites (328.7±1.8Ma); the Early Permian intrusive rocks are biotite monzogranite (290.3±2.1Ma) and quartz diorite (290.0±1.6Ma). The Early Carboniferous igneous rocks are rich in amphibole and plagioclase, belonging to the calc-alkaline, meta-aluminous series. They are enriched in large ion lithophile elements such as Rb, Ba, Th, U and Pb, and depleted in high field strength elements (e.g., Nb, Ta and Ti), and exhibit relatively depleted Sr, Nd and Hf isotopic compositions, i.e., they are resemble to the island arc magmatic rocks derived from partial melting of metasomatic mantle wedge. Compared with the Early Carboniferous igneous rocks, the Early Permian intrusive rocks are composed of plenty of biotite and alkali feldspar, which are enriched in SiO2, Na2O and K2O, and depleted in Al2O3, MgO, Fe2O3T and CaO, and Sr, Nd and Hf isotopic compositions, indicating that their magmas were originated from partial melting of a thickened juvenile crust under the post-collisional setting. Hence the Early Carboniferous and the Early Permian magmatic rocks show significant petrological and geochemical differences, which is indicative of a tectonic setting transition from the Early Carboniferous oceanic subduction to Early Permian post-collision orogeny.

图 3红山南-天木东地区岩石野外及显微照片

红山南-天木东地区岩石野外及显微照片

Figure 3.Photographs showing occurrence and micrographs of the igneous rocks from the Hongshannan-Tianmudong area

Photographs showing occurrence and micrographs of the igneous rocks from the Hongshannan-Tianmudong area

图 4红山南-天木东地区岩浆岩锆石U-Pb谐和图及加权平均年龄图

红山南-天木东地区岩浆岩锆石U-Pb谐和图及加权平均年龄图

Figure 4.Zircon U-Pb concordia diagrams and weighted mean ages of the igneous rocks from the Hongshannan-Tianmudong area

Zircon U-Pb concordia diagrams and weighted mean ages of the igneous rocks from the Hongshannan-Tianmudong area

图 5红山南-天木东地区岩浆岩地球化学特征

红山南-天木东地区岩浆岩地球化学特征

Figure 5.Geochemical characteristics of igneous rocks in the Hongshannan-Tianmudong area

Geochemical characteristics of igneous rocks in the Hongshannan-Tianmudong area

图 7东天山岩浆岩全岩Sr-Nd同位素及锆石Hf同位素组成

东天山岩浆岩全岩Sr-Nd同位素及锆石Hf同位素组成

Figure 7.Whole-rock Sr-Nd and Zircon Hf isotopic compositions of magmatic rocks in East Tianshan

Whole-rock Sr-Nd and Zircon Hf isotopic compositions of magmatic rocks in East Tianshan

图 8红山南-天木东地区岩浆岩Zr与部分元素含量二元图解

红山南-天木东地区岩浆岩Zr与部分元素含量二元图解

Figure 8.Binary diagrams of selected elements vs. Zr for the igneous rocks from the Hongshannan-Tianmudong area

Binary diagrams of selected elements vs. Zr for the igneous rocks from the Hongshannan-Tianmudong area

图 9红山南-天木东地区岩浆岩SiO2与主量元素氧化物含量二元图解

红山南-天木东地区岩浆岩SiO2与主量元素氧化物含量二元图解

Figure 9.Binary diagrams for selected major oxides vs. SiO2 contents of the igneous rocks from Hongshannan-Tianmudong area

Binary diagrams for selected major oxides vs. SiO2 contents of the igneous rocks from Hongshannan-Tianmudong area

图 11红山南-天木东地区岩浆岩构造判别图解

红山南-天木东地区岩浆岩构造判别图解

Figure 11.Tectonic discrimination diagrams of the igneous rocks from the Hongshannan-Tianmudong area

Tectonic discrimination diagrams of the igneous rocks from the Hongshannan-Tianmudong area

图 12东天山晚古生代构造演化卡通图

东天山晚古生代构造演化卡通图

Figure 12.Schematic cartoons for the Late Paleozoic tectonic evolution process of the East Tianshan

Schematic cartoons for the Late Paleozoic tectonic evolution process of the East Tianshan

表 1红山南-天木东地区岩浆岩锆石U-Pb定年分析结果

红山南-天木东地区岩浆岩锆石U-Pb定年分析结果

Table 1.Zircon U-Pb dating results for the igneous rocks from the Hongshannan-Tianmudong area

Zircon U-Pb dating results for the igneous rocks from the Hongshannan-Tianmudong area

表 2红山南-天木东地区岩浆岩主量元素(wt%)和微量元素(×10-6)含量

红山南-天木东地区岩浆岩主量元素(wt%)和微量元素(×10-6)含量

Table 2.Major (wt%) and trace (×10-6) element contents of the igneous rocks from the Hongshannan-Tianmudong area

Major (wt%) and trace (×10-6) element contents of the igneous rocks from the Hongshannan-Tianmudong area

表 3红山南-天木东地区全岩Sr-Nd同位素组成

红山南-天木东地区全岩Sr-Nd同位素组成

Table 3.Whole-rock Sr-Nd isotopic composition of the igneous rocks from the Hongshannan-Tianmudong area

Whole-rock Sr-Nd isotopic composition of the igneous rocks from the Hongshannan-Tianmudong area

表 4红山南-天木东地区岩浆岩锆石原位Hf同位素组成

红山南-天木东地区岩浆岩锆石原位Hf同位素组成

Table 4.In-situ zircon Hf isotopic composition of the igneous rocks from the Hongshannan-Tianmudong area

In-situ zircon Hf isotopic composition of the igneous rocks from the Hongshannan-Tianmudong area

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