Detrital zircon U-Pb and Hf isotopic dataset for the Central Asian Orogenic Belt, northern China

被引：3

作者：

Wang, Linxi ^{[1
]}

Huo, Ning ^{[2
,3
]}

Jiang, Guanzhe ^{[4
]}

Han, Chao ^{[1
]}

Sun, Jingxian ^{[2
]}

Huang, Hu ^{[1
,5
]}

机构：

[1] Chengdu Univ Technol, Inst Sedimentary Geol, Chengdu, Peoples R China

[2] Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing, Peoples R China

[3] Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing, Peoples R China

[4] Chinese Acad Geol Sci, Inst Geol, Beijing, Peoples R China

[5] Chengdu Univ Technol, State Key Lab Oil & Gas Reservoir Geol & Exploitat, Chengdu, Peoples R China

来源：

GEOSCIENCE DATA JOURNAL | 2024年 / 11卷 / 04期

基金：

中国国家自然科学基金;

关键词：

Central Asian Orogenic Belt; detrital zircon; Hf isotope; U-Pb age; LU-HF; TECTONIC EVOLUTION; PROVENANCE; GEOCHEMISTRY; CONSTRAINTS; JUNGGAR; CLOSURE; ROCKS; RECONSTRUCTION; GEOCHRONOLOGY;

D O I：

10.1002/gdj3.214

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

The Central Asian Orogenic Belt (CAOB) is one of the biggest accretionary orogens in the world. With the development of laser ablation-inductively coupled plasma-mass spectrometry (LA-ICP-MS), large data of detrital zircon U-Pb and Hf isotopes have been published for decades, which leads to better understanding of the tectonic evolution and geodynamics of the CAOB. We compiled the data about the information of articles, samples and their analytical methods and results, then checked and corrected. These data are available to support future research activities in the CAOB, northern China, for example, the provenance analysis, climate changes and paleogeographic reconstruction.

引用

页码：426 / 432

页数：7

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