Provenance analysis of the Late Cenozoic sediments in Dalangtan area, northwestern Qaidam Basin: evidence from detrital zircon U-Pb ages and Hf isotopes

doi:10.7605/gdlxb.2026.110

Journal of Palaeogeography（Chinese Edition） ›› 2026, Vol. 28 ›› Issue (3): 949-969. doi: 10.7605/gdlxb.2026.110

• SPECIAL TOPIC ON THE 100TH ANNIVERSARY OF PROFESSOR FENG ZENGZHAO • Previous Articles Next Articles

Provenance analysis of the Late Cenozoic sediments in Dalangtan area, northwestern Qaidam Basin: evidence from detrital zircon U-Pb ages and Hf isotopes

XIAO Menghan(), ZHENG Mianping, ZHANG Yongsheng(), HOU Xianhua, SHI Linfeng

MLR Key Laboratory of Saline Lake Resources and Environments, Institute of Mineral Resources,Chinese Academy of Geological Sciences, Beijing 100037, China

Received:2026-02-27 Revised:2026-04-15 Online:2026-06-01 Published:2026-06-05
Contact: ZHANG Yongsheng,born in 1963,Ph.D.,researcher and Ph.D. supervisor,is primarily engaged in researches on the geology of salt deposits and “oil-potash dual exploration”. E-mail: zys_601@126.com.
About author:
XIAO Menghan,born in 1999,Ph.D. candidate,is primarily engaged in researches on salinology and paleomagnetism. E-mail: xiaomenghan4869@163.com.
Supported by:
National Key Research and Development Program of China(2023YFC2906501); Geological Survey Project of the China Geological Survey(DD20230755)

柴西北晚新生代沉积源区分析:来自碎屑锆石U-Pb年龄及Hf同位素的约束^*

肖梦晗(), 郑绵平, 张永生(), 侯献华, 施林峰

中国地质科学院矿产资源研究所, 自然资源部盐湖资源与环境重点实验室, 北京 100037

通讯作者: 张永生,男,1963年生,博士,研究员,博士生导师,主要从事盐类矿床地质与“油钾兼探”研究。E-mail: zys_601@126.com。
作者简介:
肖梦晗,女,1999年生,博士研究生,主要从事盐湖学与古地磁学研究。E-mail: xiaomenghan4869@163.com。
谨以此文纪念冯增昭先生诞辰100周年。
基金资助:
*国家重点研发计划项目(2023YFC2906501); 中国地质调查局地质调查项目(DD20230755)

Abstract

Abstract:

The Qaidam Basin,on the northeastern margin of the Tibetan Plateau,preserves distinctive stratigraphic and sedimentary records of a complex basin-mountain system and multiple provenance sources. In the Dalangtan-Heibei sag of the northwestern basin,a thick Late Cenozoic gravel succession hosts a newly recognized gravel-type potash-bearing brine deposit. In this study,seven sandstone samples from different depths in boreholes CJ-2 and CJ-3 were analyzed for detrital zircon U-Pb geochronology,trace elements,and Lu-Hf isotopes. The detrital zircons are predominantly magmatic in origin,with Th/U ratios of 0.02-1.26 and REE patterns characterized by HREE enrichment,pronounced negative Eu anomalies,and positive Ce anomalies. U-Pb ages range from 213.9 to 3307 Ma and define four main age groups: 200-300 Ma,330-510 Ma,740-990 Ma,and 1.1-3.3 Ga. Provenance comparison shows that the Qigequan Formation in borehole CJ-2 was sourced mainly from the East Kunlun-Qimantagh,whereas that in borehole CJ-3 was influenced chiefly by the Altyn Tagh and the northern Qaidam margin. The Shizigou Formation shows stronger multi-source mixing: in borehole CJ-2 it records contributions from the East Kunlun-Qimantagh,northern Qaidam margin,South Qilian Mountains,and Altyn Tagh,whereas in borehole CJ-3 it was derived mainly from the East Kunlun-Qimantagh,with subordinate input from the Altyn Tagh and northern Qaidam margin. These inter-well provenance differences reflect the combined effects of lateral differentiation within the piedmont alluvial-proluvial fan system and intensified Late Cenozoic tectonic activity. The results can provide reliable age evidence for the rapid uplift of the Altun Mountains and the northern margin of the Tibetan Plateau,and offer new age constraints for exploring the gravel type potassium-bearing brine resources in the Dalangtan-Heibei sag of Qaidam Basin.

Key words: Zircon U-Pb dating, Hf isotopic, LA-ICP-MS, provenance analysis, Qaidam Basin

摘要：

柴达木盆地位于青藏高原东北缘,其特殊的地层岩性及沉积特征反映了复杂的盆山系统和多种物源区成因。柴达木盆地西北部大浪滩—黑北凹地发育一套巨厚的晚新生代砂砾石沉积层系,为新型“砂砾型”卤水钾盐矿赋存地层。本研究选取大浪滩地区柴钾2井、柴钾3井不同埋深的7个砂岩样品进行了碎屑锆石U-Pb年代学、锆石微量元素特征分析与Lu-Hf同位素研究。结果表明,研究区碎屑锆石以岩浆成因为主,Th/U值为0.02~1.26,稀土元素配分模式呈现重稀土元素相对富集、显著Eu负异常和Ce正异常。碎屑锆石U-Pb年龄总体介于213.9~3307 Ma之间,主要包括4组年龄,分别是: 200~300 Ma,330~510 Ma,740~990 Ma,1.1~3.3 Ga。通过与周缘潜在源区对比发现,柴钾2井七个泉组物源以东昆仑祁漫塔格为主,柴钾3井七个泉组主要受阿尔金山和柴北缘共同影响; 狮子沟组表现出更明显的多源混合特征,其中柴钾2井狮子沟组反映东昆仑祁漫塔格、柴北缘、南祁连山和阿尔金山共同供源,柴钾3井狮子沟组则以东昆仑祁漫塔格物源为主,同时接受阿尔金山和柴北缘的部分输入。总体上,柴钾2井、柴钾3井之间的物源差异反映出山前冲洪积扇相沉积体系的横向分异与晚新生代构造活动增强的共同控制。研究结果可为阿尔金山及青藏高原北缘快速隆升提供可靠的年龄证据,对探索柴达木盆地“砂砾型”含钾卤水资源提供了新的年代制约。

关键词: 锆石U-Pb年龄, Hf同位素, LA-ICP-MS, 物源分析, 柴达木盆地

CLC Number:

P512.2

XIAO Menghan, ZHENG Mianping, ZHANG Yongsheng, HOU Xianhua, SHI Linfeng. Provenance analysis of the Late Cenozoic sediments in Dalangtan area, northwestern Qaidam Basin: evidence from detrital zircon U-Pb ages and Hf isotopes[J]. Journal of Palaeogeography（Chinese Edition）, 2026, 28(3): 949-969.

肖梦晗, 郑绵平, 张永生, 侯献华, 施林峰. 柴西北晚新生代沉积源区分析:来自碎屑锆石U-Pb年龄及Hf同位素的约束^*[J]. 古地理学报, 2026, 28(3): 949-969.

/ / Recommend / Download Citations

URL: http://www.gdlxb.cn/EN/10.7605/gdlxb.2026.110

http://www.gdlxb.cn/EN/Y2026/V28/I3/949

Figures/Tables 15

Fig.1 Geological map and boreholes location of Qaidam Basin

Fig.2 Lithologic columns and core characteristics of boreholes CJ-2 and CJ-3 in Dalangtan area,Qaidam Basin

Fig.3 CL images of representative detrital zircon samples from boreholes CJ-2 and CJ-3 in Dalangtan area,Qaidam Basin

Fig.4 Th/U ratio from boreholes CJ-2 and CJ-3 in Dalangtan area,Qaidam Basin

Fig.5 Detrital zircon U-Pb concordia diagrams and histograms from samples of borehole CJ-2 in Dalangtan area,Qaidam Basin

Fig.6 Detrital zircon U-Pb concordia diagrams and histograms from samples of borehole CJ-3 in Dalangtan area,Qaidam Basin

Fig.7 Diagram of ε_Hf(t) vs. U-Pb age(a,b) and Hf model age histogram of detrital zircon samples from boreholes CJ-2 and CJ-3 in Dalangtan area, Qaidam Basin

Fig.8 Distribution pattern of rare earth elements of detrial zircons from borehole CJ-2 in Dalangtan area,Qaidam Basin

Fig.9 Distribution pattern of rare earth elements of detrial zircons from borehole CJ-3 in Dalangtan area,Qaidam Basin

Fig.10 Trace element lithological identification diagram of detrial zircons from boreholes CJ-2 and CJ-3 in Dalangtan area,Qaidam Basin(base map modified from Belousova et al., 2002)

Fig.11 Trace element discrimination diagrams of U/Yb-Hf, U/Yb-Y, Th/Yb-Hf and Th/Yb-Y for detrial zircons from boreholes CJ-2 and CJ-3 in Dalangtan area,Qaidam Basin(base map modified from Grimes et al., 2007)

Fig.12 Trace element discrimination diagrams of Nb/Hf-Th/U(a) and Hf/Th-Th/Nb(b) for detrial zircons from boreholes CJ-2 and CJ-3 in Dalangtan area,Qaidam Basin(base map modified from Yang et al., 2012)

Fig.13 Detrital zircon U-Pb age spectrum from boreholes CJ-2 and CJ-3 in Dalangtan area,Qaidam Basin

Fig.14 U-Pb age comparison diagram of detrital zircon between the Qigequan Formation and Shizigou Formation in Dalangtan area,Qaidam Basin

Fig.15 Detrital zircon U-Pb age spectrum from boreholes CJ-2 and CJ-3 in Dalangtan area,Qaidam Basin and its potential source areas

References 99

[1]	陈国超, 裴先治, 李瑞保, 李佐臣, 裴磊, 刘战庆, 陈有炘, 刘成军, 高景民, 魏方辉. 2013. 东昆仑洪水川地区科科鄂阿龙岩体锆石U-Pb年代学、地球化学及其地质意义. 地质学报, 87(2): 178-196.
	[Chen G C, Pei X Z, Li R B, Li Z C, Pei L, Liu Z Q, Chen Y X, Liu C J, Gao J M, Wei F H. 2013. Zircon U-Pb geochronology,geochemical characteristics and geological significance of cocoe A’Long quartz diorites body from the Hongshuichuan area in east Kunlun. Acta Geologica Sinica, 87(2): 178-196]
[2]	陈宣华, Michael W. McRivette, 李丽, 尹安, 蒋荣宝, 万景林, 李会军. 2011. 东昆仑造山带多期隆升历史的地质热年代学证据. 地质通报, 30(11): 1647-1660.
	[Chen X H, McRivette W M, Li L, Yin A, Jiang R B, Wan J L, Li H J. 2011. Thermochronological evidence for multi-phase uplifting of the East Kunlun Mountains,northern Tibetan Plateau. Geological Bulletin of China, 30(11): 1647-1660]
[3]	陈正乐, 宫红良, 李丽, 王小凤, 陈柏林, 陈宣华. 2006. 阿尔金山脉新生代隆升—剥露过程. 地学前缘, 13(4): 91-102.
	[Chen Z L, Gong H L, Li L, Wang X F, Chen B L, Chen X H. 2006. Cenozoic uplifting and exhumation process of the Altyn Tagh Mountains. Earth Science Frontiers, 13(4): 91-102]
[4]	董增产, 辜平阳, 焦和, 查显锋, 陈锐明, 张海迪. 2014. 柴北缘西端冷湖盐场北山辉长岩地球化学及年代学研究. 地质科学, 49(4): 1132-1149.
	[Dong Z C, Gu P Y, Jiao H, Zha X F, Chen R M, Zhang H D. 2014. Geochemistry and chronology of Yanchangbeishan gabrro in Lenghu area at the west segment of the north margin of Qaidam. Chinese Journal of Geology, 49(4): 1132-1149]
[5]	董增产, 辜平阳, 陈锐明, 查显锋, 张海迪. 2015. 柴北缘西端盐场北山二长花岗岩年代学、地球化学及其Hf同位素特征. 地球科学, 40(1): 130-144.
	[Dong Z C, Gu P Y, Chen R M, Zha X F, Zhang H D. 2015. Geochronology,geochemistry,and Hf isotope of Yanchangbeishan adamellite of Lenghu area in Qinghai. Earth Science, 40(1): 130-144]
[6]	侯献华, 王伟, 郑绵平, 樊馥, 李洪普, 高雪峰. 2021. 柴达木盆地西部黑北凹地—大浪滩深层卤水钾盐储卤层地震响应特征研究. 地学前缘, 28(6): 134-145. doi: 10.13745/j.esf.sf.2021.1.49
	[Hou X H, Wang W, Zheng M P, Fan F, Li H P, Gao X F. 2021. Seismic response characteristics of the Heibei Concave-Dalangtan potassium-rich deep brine reservoir in western Qaidam Basin. Earth Science Frontiers, 28(6): 134-145] doi: 10.13745/j.esf.sf.2021.1.49
[7]	李平, 高晓峰, 吕鹏瑞, 朱小辉, 陈隽璐. 2023. 祁连山—柴北缘地区岩浆活动的时空分布、成因演变及构造岩浆演化. 西北地质, 56(4): 283-317.
	[Li P, Gao X F, Lü P R, Zhu X H, Chen J L. 2023. Spatial-temporal distribution,petrogenetic evolution and tectono-magmatic evolution in Qilian Mountains and northern margin of Qaidam. Northwestern Geology, 56(4): 283-317]
[8]	李治华, 李碧乐, 王斌, 陈苏龙, 李鹏, 廖宇斌, 于润涛. 2021. 柴北缘苦水泉金矿英云闪长岩和细粒闪长岩年代学、地球化学和Hf同位素及地质意义. 岩石学报, 37(6): 1653-1673.
	[Li Z H, Li B L, Wang B, Chen S L, Li P, Liao Y B, Yu R T. 2021. Geochronology,geochemistry,Hf isotope,and their geological significance of the tonalite and fine-grained diorite from Kushuiquan gold deposit,North Qaidam. Acta Petrologica Sinica, 37(6): 1653-1673] doi: 10.18654/1000-0569/2021.06.02 URL
[9]	刘良, 康磊, 曹玉亭, 杨文强. 2015. 南阿尔金早古生代俯冲碰撞过程中的花岗质岩浆作用. 中国科学: 地球科学, 45(8): 1126-1137.
	[Liu L, Kang L, Cao Y T, Yang W Q. 2015. Early Paleozoic granitic magmatism related to the processes from subduction to collision in South Altyn,NW China. Scientia Sinica(Terrae), 45(8): 1126-1137]
[10]	彭璇, 庄玉军, 辜平阳, 时超, 何世平, 曹佰迪. 2022. 柴北缘小赛什腾山片麻状花岗岩的成因: 来自地球化学、锆石U-Pb年代学及Hf同位素约束. 西北地质, 55(4): 221-239.
	[Peng X, Zhuang Y J, Gu P Y, Shi C, He S P, Cao B D. 2022. Petrogenesis of the gneissic granite in Xiaosaishiteng Mountain,northern Qaidam: constraint from geochemistry,zircon U-Pb geochronology and Hf isotopes. Northwestern Geology, 55(4): 221-239]
[11]	彭渊, 马寅生, 刘成林, 李宗星, 孙娇鹏, 邵鹏程. 2016a. 柴北缘宗务隆构造带印支期花岗闪长岩地质特征及其构造意义. 地学前缘, 23(2): 206-221.
	[Peng Y, Ma Y S, Liu C L, Li Z X, Sun J P, Shao P C. 2016a. Geological characteristics and tectonic significance of the Indosinian granodiorites from the Zongwulong tectonic belt in North Qaidam. Earth Science Frontiers, 23(2): 206-221]
[12]	彭渊, 马寅生, 刘成林, 孙娇鹏, 胡忠亚, 牟宏良, 郑策. 2016b. 东昆仑大干沟火山岩SHRIMP锆石U-Pb测年及其地质意义. 地质通报, 35(S1): 356-363.
	[Peng Y, Ma Y S, Liu C L, Sun J P, Hu Z Y, (Mou/Mu) H L, Zheng C. 2016b. SHRIMP zircon ages of the Dagangou volcanic rocks in the eastern Kunlun orogenic belt and their implications. Geological Bulletin of China, 35(S1): 356-363]
[13]	齐瑞荣. 2012. 中祁连西段巴嘎德尔基岩体LA-ICP-MS锆石U-Pb年龄及地质意义. 沉积与特提斯地质, 32(4): 86-93.
	[Qi R R. 2012. LA-ICP-MS zircon U-Pb ages and geological implications for the Bagadeerji granitic plutons in the central Qilian Mountains,Gansu. Sedimentary Geology and Tethyan Geology, 32(4): 86-93]
[14]	祁生胜, 邓晋福, 叶占福, 刘荣, 王国良. 2013. 青海祁漫塔格地区晚泥盆世辉绿岩墙群LA-ICP-MS锆石U-Pb年龄及其构造意义. 地质通报, 32(9): 1385-1393.
	[Qi S S, Deng J F, Ye Z F, Liu R, Wang G L. 2013. LA-ICP-MS zircon U-Pb dating of Late Devonian diabase dike swarms in Qimantag area. Geological Bulletin of China, 32(9): 1385-1393]
[15]	祁晓鹏, 杨杰, 范显刚, 崔建堂, 蔡振锋, 曾献文, 魏伟, 屈小相, 翟黎明. 2016. 东昆仑东段东昆中构造混杂岩带长石山蛇绿岩年代学、地球化学特征及其构造意义. 中国地质, 43(3): 797-816.
	[Qi X P, Yang J, Fan X G, Cui J T, Cai Z F, Zeng X W, Wei W, Qu X X, Zhai L M. 2016. Age,geochemical characteristics and tectonic significance of Changshishan ophiolite in central East Kunlun tectonic mélange belt along the east section of East Kunlun Mountains. Geology in China, 43(3): 797-816]
[16]	钱涛, 李王鹏, 高万里, 何玮东, 江万, 郭迎春, 盛美. 2025. 柴北缘东段新生代沉积记录的南祁连构造隆升. 地球学报, 46(6): 1067-1081.
	[Qian T, Li W P, Gao W L, He W D, Jiang W, Guo Y C, Sheng M. 2025. South Qilian tectonic uplift in the eastern segment of the northern Qaidam Basin recorded by the Cenozoic sediments. Acta Geoscientia Sinica, 46(6): 1067-1081]
[17]	史仁灯, 杨经绥, 吴才来. 2003. 柴北缘早古生代岛弧火山岩中埃达克质英安岩的发现及其地质意义. 岩石矿物学杂志, 22(3): 229-236.
	[Shi R D, Yang J S, Wu C L. 2003. The discovery of adakitic dacite in Early Paleozoic island arc volcanic rocks on the northern margin of Qaidam Basin and its geological significance. Acta Petrologica et Mineralogica, 22(3): 229-236]
[18]	王嘉琦, 施炜, 李宗星, 钟畅. 2023. 柴达木盆地东北缘晚新生代构造隆升: 来自碎屑锆石U-Pb年代学证据. 地质论评, 69(6): 2391-2406.
	[Wang J Q, Shi W, Li Z X, Zhong C. 2023. Late Cenozoic tectonic uplift in the northeastern margin of the Qaidam Basin: evidence from detrital zircon U-Pb chronology. Geological Review, 69(6): 2391-2406]
[19]	吴才来, 郜源红, 吴锁平, 陈其龙,Joseph L.Wooden,Frank K.MAZADAB,Chris MATTINSON. 2007. 柴达木盆地北缘大柴旦地区古生代花岗岩锆石SHRIMP定年. 岩石学报, 23(8): 1861-1875.
	[Wu C L, Gao Y H, Wu S P, Chen Q L, Wooden J, Mazadab F, Mattinson C. 2007. Zircon SHRIMP U-Pb dating of granites from the Da Qaidam area in the north margin of Qaidam basin,NW China. Acta Petrologica Sinica, 23(8): 1861-1875]
[20]	吴才来, 郜源红, 吴锁平, 陈其龙,Joseph LWooden,Frank KMazadab,Chris Mattinson. 2008. 柴北缘西段花岗岩锆石SHRIMP U-Pb定年及其岩石地球化学特征. 中国科学D辑, 38(8): 930-949.
	[Wu C L, Gao Y H, Wu S P, Chen Q L, Lwooden J, Kmazadab F, Mattinson C. 2008. Zircon SHRIMP U-Pb dating of granites in the western part of northern Qaidam Basin and its petrogeochemical characteristics. Science in China(Series D), 38(8): 930-949]
[21]	吴才来, 郜源红, 雷敏, 秦海鹏, 刘春花, 李名则,B Ronald Frost,Joseph L Wooden. 2014a. 南阿尔金茫崖地区花岗岩类锆石SHRIMPU-Pb定年、Lu-Hf同位素特征及岩石成因. 岩石学报, 30(8): 2297-2323.
	[Wu C L, Gao Y H, Lei M, Qin H P, Liu C H, Li M Z, Frost B R, Wooden J L. 2014a. Zircon SHRIMP U-Pb dating,Lu-Hf isotopic characteristics and petrogenesis of the Palaeozoic granites in Mangya area,southern Altun,NW China. Acta Petrologica Sinica, 30(8): 2297-2323]
[22]	吴才来, 郜源红, 李兆丽, 雷敏, 秦海鹏, 李名则, 刘春花,Ronald B Frost,Paul T Robinson. 2014b. 都兰花岗岩锆石SHRIMP定年及柴北缘超高压带花岗岩年代学格架. 中国科学(地球科学), 44(10): 2142-2159.
	[Wu C L, Gao Y H, Li Z L, Lei M, Qin H P, Li M Z, Liu C H, Frost R, Robinson P. 2014b. Zircon SHRIMP U-Pb dating of granites from Dulan and the chronological framework of the North Qaidam UHP belt,NW China. Scientia Sinica(Terrae), 44(10): 2142-2159]
[23]	谢皓. 2024. 祁连山西段红崖子盆地新生代沉积演化及其构造意义. 中国地震局地质研究所博士学位论文.
	[Xie H. 2024. The Cenozoic sedimentary evolution and tectonic significance of the Hongyazi Basin in the western Qilian Mountains. Doctoral dissertation of Institute of Geology,China Earthquake Administration]
[24]	徐旭明, 刘广, 梁国庆. 2017. 赛什腾山一带火山岩LA-ICP-MS锆石U-Pb年龄及其地球化学特征. 新疆地质, 35(3): 250-254.
	[Xu X M, Liu G, Liang G Q. 2017. LA-ICP-MS zircon U-Pb dating and geochemical characteristics of the volcanic rocks in the area of Saishiteng Mountain. Xinjiang Geology, 35(3): 250-254]
[25]	杨明慧, 宋建军. 2002. 柴达木盆地冷湖花岗岩体岩石学初步研究. 西北地质, 35(3): 94-98.
	[Yang M H, Song J J. 2002. Petrology of the Lenghu granite mass,northwestern Qaidam basin,China. Northwestern Geology, 35(3): 94-98]
[26]	曾旭, 付锁堂, 王波, 龙国徽, 吴志雄, 崔海栋, 王琛茜. 2024. 柴达木盆地古近系下干柴沟组上段碎屑锆石U-Pb测年及盆山耦合探讨. 地质学报, 98(1): 79-105.
	[Zeng X, Fu S T, Wang B, Long G H, Wu Z X, Cui H D, Wang C X. 2024. Detrital zircon U-Pb dating of the Paleogene Lower Ganchaigou Formation in the Qaidam Basin and discussion of basin-mountain coupling. Acta Geologica Sinica, 98(1): 79-105]
[27]	张涛, 宋春晖, 王亚东, 郑海军, 张志高, 吴松, 孟庆泉, 方小敏. 2012. 柴达木盆地西部地区晚新生代构造变形及其意义. 地学前缘, 19(5): 312-321.
	[Zhang T, Song C H, Wang Y D, Zheng H J, Zhang Z G, Wu S, Meng Q Q, Fang X M. 2012. The Late Cenozoic tectonic deformation in the Western Qaidam Basin and its implications. Earth Science Frontiers, 19(5): 312-321]
[28]	张照伟, 李文渊, 王亚磊, 高永宝. 2015. 南祁连化隆地区下什堂含铜镍矿基性—超基性岩体成因研究: 锆石年代学、地球化学和Sr-Nd同位素约束. 岩石学报, 31(9): 2539-2548.
	[Zhang Z W, Li W Y, Wang Y L, Gao Y B. 2015. The genesis study on Xiashentang basic-ultrabasic intrusion associated with Ni-Cu mineralization in Hualong,southern Qilian Mountains: zircon geochronology,geochemistry and Sr-Nd isotopic constraints. Acta Petrologica Sinica, 31(9): 2539-2548]
[29]	赵菲菲, 孙丰月, 刘金龙. 2017. 东昆仑马尼特地区片麻状花岗闪长岩锆石U-Pb年代学、地球化学及其构造背景. 地球科学, 42(6): 927-940,1044.
	[Zhao F F, Sun F Y, Liu J L. 2017. Zircon U-Pb geochronology and geochemistry of the gneissic granodiorite in Manite area from East Kunlun,with implications for geodynamic setting. Earth Science, 42(6): 927-940,1044]
[30]	赵文涛, 刘少峰, 陈敏. 2020. 柴北缘乌兰北部地区滩间山群碎屑锆石年代学、Hf同位素组成及其地质意义. 中国矿业, 29(S1): 279-283.
	[Zhao W T, Liu S F, Chen M. 2020. Detrital zircons chronology,Hf isotopes and its geological significance from Tanjianshan group in the north Wulan terrane,north Qaidam. China Mining Magazine, 29(S1): 279-283]
[31]	郑绵平, 侯献华, 于常青, 李洪普, 尹宏伟, 张震, 邓小林, 张永生, 郭廷峰, 韦钊, 王绪本, 安莲英, 乜贞, 谭筱虹, 张雪飞, 牛新生. 2015. 成盐理论引领我国找钾取得重要进展. 地球学报, 36(2): 129-139.
	[Zheng M P, Hou X H, Yu C Q, Li H P, Yin H W, Zhang Z, Deng X L, Zhang Y S, Guo T F, Wei Z, Wang X B, An L Y, Nie Z, Tan X H, Zhang X F, Niu X S. 2015. The leading role of salt formation theory in the breakthrough and important progress in potash deposit prospecting. Acta Geoscientica Sinica, 36(2): 129-139]
[32]	钟海仁, 孙艳, 赵芝, 王成辉. 2020. 重庆南川铝土矿物源分析: 碎屑锆石U-Pb定年、Hf同位素和锆石微量元素示踪. 地质学报, 94(5): 1505-1524.
	[Zhong H R, Sun Y, Zhao Z, Wang C H. 2020. Provenance of bauxite deposits in the Nanchuan district,Chongqing: evidence from U-Pb dating,Hf isotopes and trace elements in detrital zircons. Acta Geologica Sinica, 94(5): 1505-1524]
[33]	朱小辉, 陈丹玲, 刘良, 赵姣, 张乐. 2014. 柴北缘绿梁山地区早古生代弧后盆地型蛇绿岩的年代学、地球化学及大地构造意义. 岩石学报, 30(3): 822-834.
	[Zhu X H, Chen D L, Liu L, Zhao J, Zhang L. 2014. Geochronology,geochemistry and significance of the Early Paleozoic back-arc type ophiolite in Lvliangshan area,North Qaidam. Acta Petrologica Sinica, 30(3): 822-834]
[34]	庄玉军, 辜平阳, 李培庆, 何世平, 陈锐明, 查显锋. 2019. 柴北缘构造带欧龙布鲁克地块西北缘辉长岩脉地球化学、年代学及Hf同位素特征. 地质通报, 38(11): 1801-1812.
	[Zhuang Y J, Gu P Y, Li P Q, He S P, Chen R M, Zha X F. 2019. Geochemistry,geochronology and Hf isotopic compositions of metagabbro dykes on the northwestern margin of Oulongbuluke micro-block on the northern margin of Qaidam Basin. Geological Bulletin of China, 38(11): 1801-1812]
[35]	庄玉军, 辜平阳, 高永伟, 彭璇, 何世平, 李普涛. 2020. 柴北缘赛什腾中二叠世辉长岩成因及其对宗务隆洋盆俯冲时限的制约. 岩石矿物学杂志, 39(6): 718-734.
	[Zhuang Y J, Gu P Y, Gao Y W, Peng X, He S P, Li P T. 2020. Petrogenesis of Middle Permian gabbro in Saishiteng Mountain of the northern Qaidam Basin and its constraint to the time of Zongwulong Ocean subduction. Acta Petrologica et Mineralogica, 39(6): 718-734]
[36]	Andersen T. 2002. Correction of common lead in U-Pb analyses that do not report ²⁰⁴Pb. Chemical Geology,192: 59-79.
[37]	Belousova E, Griffin W, O’Reilly S Y, Fisher N. 2002. Igneous zircon: Trace element composition as an indicator of source rock type. Contributions to Mineralogy and Petrology, 143(5): 602-622. doi: 10.1007/s00410-002-0364-7 URL
[38]	Bhatia M R, Crook K A W. 1986. Trace element characteristics of graywackes and tectonic setting discrimination of sedimentary basins. Contributions to Mineralogy and Petrology, 92(2): 181-193. doi: 10.1007/BF00375292 URL
[39]	Bouvier A, Vervoort J D, Patchett P J. 2008. The Lu-Hf and Sm-Nd isotopic composition of CHUR: constraints from unequilibrated chondrites and implications for the bulk composition of terrestrial planets. Earth and Planetary Science Letters,273: 48-57.
[40]	Cao J, Hu K, Wang K, Bian L Z, Liu Y T, Yang S Y, Wang L Q, Chen Y. 2008. Possible origin of 25-norhopanes in Jurassic organic-poor mudstones from the northern Qaidam Basin(NW China). Organic Geochemistry, 39(8): 1058-1065. doi: 10.1016/j.orggeochem.2008.01.021 URL
[41]	Cawood P A, Wang Y J, Xu Y J, Zhao G C. 2013. Locating South China in Rodinia and Gondwana: a fragment of greater India lithosphere. Geology,41: 903-906.
[42]	Chang H, Ao H, An Z S, Fang X M, Song Y G, Qiang X K. 2012. Magnetostratigraphy of the Suerkuli Basin indicates Pliocene(3.2 Ma)activity of the middle Altyn Tagh Fault,northern Tibetan Plateau. Journal of Asian Earth Sciences,44: 169-175.
[43]	Chen A D, Zheng M P, Shi L F, Wang H L, Xu J M. 2017. Magnetostratigraphy of deep drilling core 15YZK 01 in the northwestern Qaidam Basin(NE Tibetan Plateau): tectonic movement,salt deposits and their link to Quaternary glaciation. Quaternary International,436: 201-211.
[44]	Chen H J, Wang N, Wu C L, Lei M, Zheng K, Zhang X, Gao D. 2018. Geochemistry,zircon U-Pb dating and Hf isotopic characteristics of Neoproterozoic granitoids in the Yaganbuyang area,Altyn Tagh,NW China. Acta Geologica Sinica(English Edition), 92(4): 1366-1383.
[45]	Cheng F, Jolivet M, Hallot E, Zhang D W, Zhang C H, Guo Z J. 2017. Tectono-magmatic rejuvenation of the Qaidam craton,northern Tibet. Gondwana Research,49: 248-263.
[46]	Clark M K. 2011. Early Tibetan Plateau uplift history eludes. Geology, 39(10): 991-992. doi: 10.1130/focus102011.1 URL
[47]	Cowgill E, Yin A, Harrison T M, Wang X F. 2003. Reconstruction of the Altyn Tagh fault based on U-Pb geochronology: role of back thrusts,mantle sutures,and heterogeneous crustal strength in forming the Tibetan Plateau. Journal of Geophysical Research: Solid Earth,108: 2002JB002080.
[48]	Duvall A R, Clark M K, Kirby E, Farley K A, Craddock W H, Li C Y, Yuan D Y. 2013. Low-temperature thermochronometry along the Kunlun and Haiyuan Faults,NE Tibetan Plateau: evidence for kinematic change during late-stage orogenesis. Tectonics, 32(5): 1190-1211. doi: 10.1002/tect.v32.5 URL
[49]	Fang X M, Zhang W L, Meng Q Q, Gao J P, Wang X M, King J, Song C H, Dai S, Miao Y F. 2007. High-resolution magnetostratigraphy of the Neogene Huaitoutala section in the eastern Qaidam Basin on the NE Tibetan Plateau,Qinghai Province,China and its implication on tectonic uplift of the NE Tibetan Plateau. Earth and Planetary Science Letters, 258(1-2): 293-306. doi: 10.1016/j.epsl.2007.03.042 URL
[50]	Gao J, Fang X, Song C, Li S, Xue J. 2011. Tectonic-thermo events of northern Tibetan Plateau: evidence from detrital apatite fission-track data in western Qaidam Basin. Journal of Jilin University, 41(5): 1466-1475.
[51]	Gehrels G E, Yin A, Wang X F. 2003a. Detrital-zircon geochronology of the northeastern Tibetan Plateau. Geological Society of America Bulletin,115: 881-896.
[52]	Gehrels G E, Yin A, Wang X F. 2003b. Magmatic history of the northeastern Tibetan Plateau. Journal of Geophysical Research: Solid Earth,108: 2002JB001876.
[53]	Gehrels G E, Valencia V A, Ruiz J. 2008. Enhanced precision,accuracy,efficiency,and spatial resolution of U-Pb ages by laser ablation: multicollector-nductively coupled plasma-mass spectrometry. Geochemistry,Geophysics, Geosystems,9: 2007GC001805.
[54]	Griffin W L, Pearson N J, Belousova E, Jackson S E, van Achterbergh E, O’Reilly S Y, Shee S R. 2000. The Hf isotope composition of cratonic mantle: LAM-MC-ICPMS analysis of zircon megacrysts in kimberlites. Geochimica et Cosmochimica Acta, 64(1): 133-147. doi: 10.1016/S0016-7037(99)00343-9 URL
[55]	Grimes C B, John B E, Kelemen P B, Mazdab F K, Wooden J L, Cheadle M J, Hanghøj K, Schwartz J J. 2007. Trace element chemistry of zircons from oceanic crust: a method for distinguishing detrital zircon provenance. Geology, 35(7): 643-646. doi: 10.1130/G23603A.1 URL
[56]	Hanson A D, Ritts B D, Zinniker D, Moldowan J M, Biffi U. 2001. Upper Oligocene lacustrine source rocks and petroleum systems of the northern Qaidam Basin,northwest China. AAPG Bulletin, 85(4): 601-619. doi: 10.1306/8626C95B-173B-11D7-8645000102C1865D URL
[57]	Harrison T M, Copeland P, Kidd W, Yin A. 1992. Raising Tibet. Science,255: 1663-1670.
[58]	He P J, Song C H, Wang Y D, Chen L H, Chang P F, Wang Q Q, Ren B. 2017. Cenozoic exhumation in the Qilian Shan,northeastern Tibetan Plateau: evidence from detrital fission track thermochronology in the Jiuquan Basin. Journal of Geophysical Research: Solid Earth, 122(8): 6910-6927. doi: 10.1002/jgrb.v122.8 URL
[59]	He P J, Song C H, Wang Y D, Meng Q Q, Chen L H, Yao L J, Huang R H, Feng W, Chen S. 2018. Cenozoic deformation history of the Qilian Shan(northeastern Tibetan Plateau)constrained by detrital apatite fission-track thermochronology in the northeastern Qaidam Basin. Tectonophysics,749: 1-11.
[60]	He P J, Song C H, Wang Y D, Meng Q Q, Wang D C, Feng Y, Chen L H, Feng W. 2020. Early Cenozoic exhumation in the Qilian Shan,northeastern margin of the Tibetan Plateau: insights from detrital apatite fission track thermochronology. Terra Nova, 32(6): 415-424. doi: 10.1111/ter.v32.6 URL
[61]	Hoskin P W, Ireland T R. 2000. Rare earth element chemistry of zircon and its use as a provenance indicator. Geology, 28(7): 627-630. doi: 10.1130/0091-7613(2000)28<627:REECOZ>2.0.CO;2 URL
[62]	Hoskin P W, Schaltegger U. 2003. The composition of zircon and igneous and metamorphic petrogenesis. Reviews in Mineralogy and Geochemistry,53: 27-62.
[63]	Jian X, Guan P, Zhang W, Feng F. 2013. Geochemistry of Mesozoic and Cenozoic sediments in the northern Qaidam Basin,northeastern Tibetan Plateau: implications for provenance and weathering. Chemical Geology,360: 74-88.
[64]	Jian X, Weislogel A, Pullen A, Shang F. 2020. Formation and evolution of the Eastern Kunlun Range,northern Tibet: evidence from detrital zircon U-Pb geochronology and Hf isotopes. Gondwana Research,83: 63-79.
[65]	Jian X, Guan P, Fu L, Zhang W, Shen X T, Fu H J, Wang L. 2024. Detrital zircon geochronology and provenance of Cenozoic deposits in the Qaidam Basin,northern Tibetan Plateau: an overview with new data,implications and perspectives. Marine and Petroleum Geology,159: 106566.
[66]	Jolivet M, Brunel M, Seward D, Xu Z, Yang J, Roger F, Tapponnier P, Malavieille J, Arnaud N, Wu C. 2001. Mesozoic and Cenozoic tectonics of the northern edge of the Tibetan Plateau: fission-track constraints. Tectonophysics, 343(1-2): 111-134. doi: 10.1016/S0040-1951(01)00196-2 URL
[67]	Li W, Neubauer F, Liu Y J, Genser J, Ren S M, Han G Q, Liang C Y. 2013. Paleozoic evolution of the Qimantagh magmatic arcs,Eastern Kunlun Mountains: constraints from zircon dating of granitoids and modern river sands. Journal of Asian Earth Sciences,77: 183-202.
[68]	Liu Y J, Genser J, Ge X H, Neubauer F, Friedl G, Chang L H, Ren S M, Handler R. 2003. ⁴⁰Ar/³⁹Ar age evidence for Altyn fault tectonic activities in western China. Chinese Science Bulletin, 48(18): 2024-2030. doi: 10.1007/BF03183998 URL
[69]	Liu Y S, Gao S, Hu Z C, Gao C G, Zong K Q, Wang D B. 2010. Continental and oceanic crust recycling-induced melt-peridotite interactions in the Trans-North China Orogen: U-Pb dating,Hf isotopes and trace elements in zircons from mantle xenoliths. Journal of Petrology, 51(1-2): 537-571. doi: 10.1093/petrology/egp082 URL
[70]	Lu H J, Ye J C, Guo L C, Pan J W, Xiong S F, Li H B. 2019. Towards a clarification of the provenance of Cenozoic sediments in the northern Qaidam Basin. Lithosphere, 11(2): 252-272. doi: 10.1130/L1037.1 URL
[71]	Ludwig K R. 2003. User’s Manual for Isoplot 3.0:A Geochronological Toolkit for Microsoft Excel. Berkeley,California: Berkeley Geochronology Center Special Publication 4: 71.
[72]	McLennan S M. 2018. Rare earth elements in sedimentary rocks:influence of provenance and sedimentary processes. In: Geochemistry and Mineralogy of Rare Earth Elements. De Gruyter: 169-200.
[73]	Morel M, Nebel O, Nebel-Jacobsen Y J, Miller J S, Vroon P Z. 2008. Hafnium isotope characterization of the GJ-1 zircon reference material by solution and laser-ablation MC-ICPMS. Chemical Geology, 255(1-2): 231-235. doi: 10.1016/j.chemgeo.2008.06.040 URL
[74]	Niu M L, Cai Q R, Li X C, Yakymchuk C, Wu Q, Yuan X Y, Sun Y. 2021. Early Paleozoic tectonic transition from oceanic to continental subduction in the North Qaidam tectonic belt: constraints from geochronology and geochemistry of syncollisional magmatic rocks. Gondwana Research,91: 58-80.
[75]	Ritts B D, Biffi U. 2001. Mesozoic northeast Qaidam Basin: response to contractional reactivation of the Qilian Shan,and implications for the extent of Mesozoic intracontinental deformation in central Asia. Paleozoic and Mesozoic Tectonic Evolution of Central and Eastern Asia: From Continental Assembly to Intracontinental Deformation. Geological Society of America Memoir,194: 293-316.
[76]	Royden L H, Burchfiel B C, van der Hilst R D. 2008. The geological evolution of the Tibetan Plateau. Science,321: 1054-1058.
[77]	Scherer E, Münker C, Mezger K. 2001. Calibration of the lutetium-hafnium clock. Science,293: 683-687.
[78]	Song K, Ding Q F, Zhang Q, Cheng L, Han Y, Liu F. 2020. Zircon U-Pb geochronology,Hf isotopes,and whole-rock geochemistry of Hongshuihe Early to Middle Triassic quartz diorites and granites in the Eastern Kunlun Orogen,NW China: implication for petrogenesis and geodynamics. Geological Journal,55: 1507-1528.
[79]	Song S G, Su L, Li X H, Niu Y L, Zhang L F. 2012. Grenville-age orogenesis in the Qaidam-Qilian block: the link between South China and Tarim. Precambrian Research,220: 9-22.
[80]	Sun G J, Zhang J J, Long S, Liu X W, Yang X, Liu Y H. 2010. Mesozoic-Cenozoic tectonic evolution in northwestern Qaidam Basin. Natural Gas Geoscience, 21(2): 212-217.
[81]	Sun J M, Zhu R X, An Z S. 2005. Tectonic uplift in the northern Tibetan Plateau since 13.7 Ma ago inferred from molasse deposits along the Altyn Tagh Fault. Earth and Planetary Science Letters,235: 641-653.
[82]	Tapponnier P, Molnar P. 1977. Active faulting and tectonics in China. Journal of Geophysical Research, 82(20): 2905-2930. doi: 10.1029/JB082i020p02905 URL
[83]	Taylor S R, McLennan S M. 1985. The continental crust: its composition and evolution. Oxford: Blackwell Scientific Publications.
[84]	Tung K, Yang H J, Yang H Y, Liu D Y, Zhang J X, Wan Y S, Tseng C Y. 2007. SHRIMP U-Pb geochronology of the zircons from the Precambrian basement of the Qilian Block and its geological significances. Chinese Science Bulletin, 52(19): 2687-2701. doi: 10.1007/s11434-007-0356-0 URL
[85]	Wang L, MacLennan S A, Cheng F. 2020. From a proximal-deposition-dominated basin sink to a significant sediment source to the Chinese Loess Plateau: insight from the quantitative provenance analysis on the Cenozoic sediments in the Qaidam Basin,northern Tibetan Plateau. Palaeogeography,Palaeoclimatology, Palaeoecology,556: 109883.
[86]	Wang Y D, Zheng J J, Zheng Y W, Liu X W, Sun G Q. 2015. Paleocene-Early Eocene uplift of the Altyn Tagh Mountain: evidence from detrital zircon fission track analysis and seismic sections in the northwestern Qaidam Basin. Journal of Geophysical Research: Solid Earth,120: 8534-8550.
[87]	Wu C, Li J, Ding L. 2021. Low-temperature thermochronology constraints on the evolution of the Eastern Kunlun Range,northern Tibetan Plateau. Geosphere, 17(4): 1193-1213. doi: 10.1130/GES02358.1 URL
[88]	Wu C L, Chen H J, Wu D, Ernst W G. 2018. Paleozoic granitic magmatism and tectonic evolution of the South Altun block,NW China: constraints from zircon U-Pb dating and Lu-Hf isotope geochemistry. Journal of Asian Earth Sciences,160: 168-199.
[89]	Xia W C, Zhang N, Yuan X P, Fan L S, Zhang B S. 2001. Cenozoic Qaidam Basin,China: a stronger tectonic inversed,extensional rifted basin. AAPG Bulletin,85: 715-736.
[90]	Xiao W J, Windley B F, Yong Y, Yan Z, Yuan C, Liu C Z, Li J L. 2009. Early Paleozoic to Devonian multiple-accretionary model for the Qilian Shan,NW China. Journal of Asian Earth Sciences,35: 323-333.
[91]	Xiong Q, Zheng J P, Griffin W L, O’Reilly S Y, Pearson N J. 2012. Decoupling of U-Pb and Lu-Hf isotopes and trace elements in zircon from the UHP North Qaidam orogen,NE Tibet(China): tracing the deep subduction of continental blocks. Lithos,155: 125-145.
[92]	Yang J H, Cawood P A, Du Y S, Huang H, Hu L S. 2012. Detrital record of Indosinian mountain building in SW China: provenance of the Middle Triassic turbidites in the Youjiang Basin. Tectonophysics,574: 105-117.
[93]	Yin A, Harrison T M. 2000. Geologic evolution of the Himalayan-Tibetan Orogen. Annual Review of Earth and Planetary Sciences, 28(1): 211-280.
[94]	Yin A, Rumelhart P E, Butler R, Cowgill E, Harrison T M, Foster D A, Ingersoll R V, Zhang Q, Zhou X Q, Wang X F, Hanson A, Raza A. 2002. Tectonic history of the Altyn Tagh fault system in northern Tibet inferred from Cenozoic sedimentation. Geological Society of America Bulletin, 114(10): 1257-1295. doi: 10.1130/0016-7606(2002)114<1257:THOTAT>2.0.CO;2 URL
[95]	Yue Y, Ritts B D, Graham S A, Wooden J L, Gehrels G E, Zhang Z. 2004. Slowing extrusion tectonics: lowered estimate of post-Early Miocene slip rate for the Altyn Tagh fault. Earth and Planetary Science Letters, 217(1-2): 111-122. doi: 10.1016/S0012-821X(03)00544-2 URL
[96]	Zhang W, Li B, Yan M. 2022. Anisotropy of magnetic susceptibility reveals Late Cenozoic tectonic processes in the western Qaidam Basin,NE Tibetan Plateau. Frontiers in Earth Science,10: 845924.
[97]	Zhao J, Zeng X, Tian J, Hu C, Wang D, Yan Z, Wang K, Zhao X. 2020a. Provenance and paleogeography of the Jurassic northwestern Qaidam Basin(NW China): evidence from sedimentary records and detrital zircon geochronology. Journal of Asian Earth Sciences,190: 104060.
[98]	Zhao X, Zhao J, Zeng X, Tian J, Guo Z, Wang C, Wang D, Hu C. 2020b. Early-Middle Jurassic paleogeography reconstruction in the western Qaidam Basin: insights from sedimentology and detrital zircon geochronology. Marine and Petroleum Geology,118: 104445.
[99]	Zhuang G, Hourigan J K, Ritts B D, Kent-Corson M L. 2011. Cenozoic multiple-phase tectonic evolution of the northern Tibetan Plateau: constraints from sedimentary records from Qaidam Basin,Hexi Corridor,and Subei Basin,northwest China. American Journal of Science, 311(2): 116-152. doi: 10.2475/02.2011.02 URL

Please choose a citation manager

Content to export