鄂尔多斯盆地西北部下白垩统物源定量分析研究

刘持恒, 李子颖, 贺锋, 张字龙, 李振成, 凌明星, 刘瑞萍

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地学前缘 ›› 2024, Vol. 31 ›› Issue (3) : 80-99. DOI: 10.13745/j.esf.sf.2023.6.22
沉积作用与沉积环境

鄂尔多斯盆地西北部下白垩统物源定量分析研究

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Quantitative analysis of provenance in the Lower Cretaceous of the northwestern Ordos Basin

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摘要

下白垩统是鄂尔多斯盆地晚中生代的一个重要构造层,同时也是近年来新发现砂岩型铀矿的重要层位。恢复该时期的源-汇系统对认识燕山运动晚期在华北克拉通西部的构造-沉积响应、古气候转变和盆地内砂岩铀矿的富集规律均有较大的帮助。本文通过对鄂尔多斯盆地西北部下白垩统进行古流向测量、不同层位碎屑锆石U-Pb测年,优化周缘潜在物源区锆石U-Pb年龄数据集的汇编方案,定量计算出各物源区对盆内的碎屑贡献比例,恢复了鄂尔多斯盆地西北部早白垩世的源-汇系统。研究结果表明,鄂尔多斯盆地西北部下白垩统中碎屑锆石具有1.79~1.64 Ga、2.02~1.82 Ga和2.58~2.45 Ga 3个稳定的前寒武纪年龄峰值,以及336~257 Ma和476~425 Ma两个稳定的显生宙年龄峰值。定量的物源分析结果表明,阴山、狼山、桌子山-贺兰山和阿拉善地区以不同的贡献比例为研究区提供物源,具多物源同时供给的特征。阴山在整个早白垩世一直是主要的物源供给区,与狼山共同向盆地内部提供河流相沉积。阿拉善地区则通过原地风蚀将物质从桌子山北部和贺兰山顶以风沙搬运的方式带入鄂尔多斯盆地,在洛河-罗汉洞沉积期共同构成了研究区风成与水成交替的沉积特征。

Abstract

The Lower Cretaceous represents a significant structural layer in the Ordos Basin, particularly notable for the emergence of sandstone-type uranium deposits in recent years. Understanding the source-sink dynamics during this period offers valuable insights into the tectonic-sedimentary processes triggered by the late Yanshanian orogeny in the western North China Craton, the paleoclimate transition, and the enrichment patterns of sandstone uranium deposits within the Ordos Basin. In this study, we conducted paleocurrent azimuth measurements and detrital zircon U-Pb dating across various strata of the Lower Cretaceous in the northwestern Ordos Basin. Furthermore, we refined the compilation approach for the zircon U-Pb age dataset in the potential provenance area surrounding the basin. Utilizing quantitative analyses, we assessed the detrital contributions from each provenance to the basin. Subsequently, the source-sink system of the Lower Cretaceous in the northwestern Ordos Basin was reconstructed. The results delineate the U-Pb ages of detrital zircons from the Lower Cretaceous into three primary groups: 1.79-1.64 Ga, 2.02-1.82 Ga, and 2.58-2.45 Ga, corresponding to Precambrian ages. Additionally, two major age groups of 336-257 Ma and 476-425 Ma signify Phanerozoic ages. Through quantitative provenance analysis, we identified the Yinshan, Langshan, Zhuozishan-Helanshan, and Alxa regions as collective sediment contributors to the study area, each with varying contribution ratios, indicating a diverse provenance supply. Our study suggests that during the Early Cretaceous, the Yinshan and Langshan regions primarily acted as provenance areas, supplying fluvial deposits to the basin’s interior. In contrast, the Alashan area transported sediments from the northern part of Zhuozishan and the Helanshan peak into the Ordos Basin through aeolian processes. This phenomenon led to the deposition of alternating eolian and fluvial formations in the study area during the Luohe-Lohandong period in the Early Cretaceous.

关键词

鄂尔多斯盆地 / 碎屑锆石U-Pb年龄 / 物源分析 / 古流向 / 砂岩型铀矿 / 源-汇系统

Key words

Ordos Basin / detrital zircon U-Pb age / provenance analysis / paleocurrent / sandstone-type uranium deposit / source-sink system

中图分类号

P544.4;P534.53;P597.3;P619.14

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刘持恒 , 李子颖 , 贺锋 , 等. 鄂尔多斯盆地西北部下白垩统物源定量分析研究. 地学前缘. 2024, 31(3): 80-99 https://doi.org/10.13745/j.esf.sf.2023.6.22
Chiheng LIU, Ziying LI, Feng HE, et al. Quantitative analysis of provenance in the Lower Cretaceous of the northwestern Ordos Basin[J]. Earth Science Frontiers. 2024, 31(3): 80-99 https://doi.org/10.13745/j.esf.sf.2023.6.22

参考文献

列表( 原文顺序 | 文献年度倒序 | 文中引用次数倒序 ) 可视化分析
[1]
SÒMME T O, HELLAND-HANSEN W, MARTINSEN O J, et al. Relationships between morphological and sedimentological parameters in source-to-sink systems: a basis for predicting semi-quantitative characteristics in subsurface systems[J]. Basin Research, 2009, 21(4): 361-387.
本文引用 [1]
[2]
邓军, 王庆飞, 高帮飞, 等. 鄂尔多斯盆地多种能源矿产分布及其构造背景[J]. 地球科学: 中国地质大学学报, 2006, 31(3): 330-336.
本文引用 [1]
[3]
刘池洋, 赵红格, 谭成仟, 等. 多种能源矿产赋存与盆地成藏(矿)系统[J]. 石油与天然气地质, 2006, 27(2): 131-142.
本文引用 [1]
[4]
杨明慧, 刘池洋. 鄂尔多斯中生代陆相盆地层序地层格架及多种能源矿产聚集[J]. 石油与天然气地质, 2006, 27(4): 563-570.
本文引用 [1]
[5]
王毅, 杨伟利, 邓军, 等. 多种能源矿产同盆共存富集成矿(藏)体系与协同勘探: 以鄂尔多斯盆地为例[J]. 地质学报, 2014, 88(5): 815-824.
本文引用 [1]
[6]
ZHANG Y Q, SHI W, DONG S W. Changes of late Mesozoic tectonic regimes around the Ordos Basin (North China) and their geodynamic implications[J]. Acta Geologica Sinica(English Edition), 2011, 85(6): 1254-1276.
本文引用 [2]
[7]
何登发, 包洪平, 开百泽, 等. 鄂尔多斯盆地及其邻区关键构造变革期次及其特征[J]. 石油学报, 2021, 42(10): 1255-1269.
本文引用 [2]
[8]
刘池洋, 王建强, 张东东, 等. 鄂尔多斯盆地油气资源丰富的成因与赋存-成藏特点[J]. 石油与天然气地质, 2021, 42(5): 1011-1029.
本文引用 [1]
[9]
WU C H, RODRÍGUEZ-LÓPEZ J P, SANTOSH M. Plateau archives of lithosphere dynamics, cryosphere and paleoclimate: the formation of Cretaceous desert basins in East Asia[J]. Geoscience Frontiers, 2022, 13(6): 101454.
本文引用 [1]
[10]
张天福, 苗培森, 程先钰, 等. 鄂尔多斯盆地早白垩世含铀岩系的新发现及其层序地层[J]. 大地构造与成矿学, 2020, 44(4): 633-647.
本文引用 [1]
[11]
REN Y S, YANG X Y, MIAO P S, et al. Mineralogical and geochemical research on Pengyang deposit: a peculiar eolian sandstone-hosted uranium deposit in the southwest of Ordos Basin[J]. Ore Geology Reviews, 2022, 141: 104571.
本文引用 [1]
[12]
刘鑫扬, 贺锋, 剡鹏兵, 等. 鄂尔多斯盆地下白垩统砂岩型铀矿找矿方向[J]. 铀矿地质, 2022, 38(2): 168-180.
本文引用 [3]
[13]
王龙辉, 剡鹏兵, 焦养泉, 等. 鄂尔多斯盆地北部下白垩统铀成矿模式[J]. 地质科技通报, 2023, 42(3): 222-233.
本文引用 [1]
[14]
CHEN Y, LI J G, MIAO P S, et al. U-Pb ages and Hf isotopes of detrital zircons from the Cretaceous succession in the southwestern Ordos Basin, northern China: implications for provenance and tectonic evolution[J]. Journal of Asian Earth Sciences, 2021, 219: 104896.
本文引用 [1]
[15]
李姣莉, 王建强, 彭恒, 等. 鄂尔多斯盆地南部下白垩统宜君组碎屑锆石U-Pb年龄及物源意义[J]. 沉积学报, 2023, 41(5): 1609-1623.
本文引用 [1]
[16]
雷开宇, 刘池洋, 张龙, 等. 鄂尔多斯盆地北部中生代中晚期地层碎屑锆石U-Pb定年与物源示踪[J]. 地质学报, 2017, 91(7): 1522-1541.
本文引用 [1]
[17]
MOECHER D, SAMSON S. Differential zircon fertility of source terranes and natural bias in the detrital zircon record: implications for sedimentary provenance analysis[J]. Earth and Planetary Science Letters, 2006, 247(3/4): 252-266.
本文引用 [3]
[18]
MALUSÀ M G, CARTER A, LIMONCELLI M, et al. Bias in detrital zircon geochronology and thermochronometry[J]. Chemical Geology, 2013, 359: 90-107.
本文引用 [2]
[19]
郭佩, 刘池洋, 王建强, 等. 碎屑锆石年代学在沉积物源研究中的应用及存在问题[J]. 沉积学报, 2017, 35(1): 46-56.
本文引用 [2]
[20]
VERMEESCH P. Multi-sample comparison of detrital age distributions[J]. Chemical Geology, 2013, 341: 140-146.
本文引用 [1]
[21]
SUNDELL K E, SAYLOR J E. Unmixing detrital geochronology age distributions[J]. Geochemistry, Geophysics, Geosystems, 2017, 18(8): 2872-2886.
本文引用 [3]
[22]
刘池洋, 赵红格, 桂小军, 等. 鄂尔多斯盆地演化-改造的时空坐标及其成藏(矿)响应[J]. 地质学报, 2006, 80(5): 617-638.
本文引用 [1]
[23]
RITTS B D, WEISLOGEL A, GRAHAM S A, et al. Mesozoic tectonics and sedimentation of the giant poly-phase nonmarine intraplate Ordos Basin, western North China Block[J]. International Geology Review, 2009, 51: 95-115.
本文引用 [1]
[24]
翟明国. 鄂尔多斯地块是破解华北早期大陆形成演化和构造体制谜团的钥匙[J]. 科学通报, 2021, 66(26): 3441-3461.
本文引用 [1]
[25]
ZHANG Y Q. Jurassic tectonics of North China: a synthetic view[J]. Acta Geologica Sinica (English Edition), 2008, 82(2): 310-326.
本文引用 [1]
[26]
ZHANG Y Q, QIU E K, DONG S W, et al. Late Mesozoic intracontinental deformation and magmatism in North and NE China in response to multi-plate convergence in NE Asia: an overview and new view[J]. Tectonophysics, 2022, 835: 229377.
本文引用 [1]
[27]
赵红格, 刘池洋, 王锋, 等. 贺兰山隆升时限及其演化[J]. 中国科学(D辑: 地球科学), 2007, 37(增刊1): 185-192.
本文引用 [2]
[28]
马静辉, 何登发. 贺兰山构造带及邻区中—新生代构造事件: 来自不整合面和裂变径迹的约束[J]. 岩石学报, 2019, 35(4): 1121-1142.
本文引用 [1]
[29]
YU Q, REN Z L, LI R X, et al. Cooling history of the southwestern Ordos Basin (northern China) since Late Jurassic: insights from thermochronology and geothermometry[J]. Journal of Asian Earth Sciences, 2021, 219: 104895.
本文引用 [1]
[30]
王建强, 刘池洋, 闫建萍, 等. 鄂尔多斯盆地南部渭北隆起发育时限及其演化[J]. 兰州大学学报(自然科学版), 2010, 46(4): 22-29.
本文引用 [1]
[31]
任战利, 崔军平, 郭科, 等. 鄂尔多斯盆地渭北隆起抬升期次及过程的裂变径迹分析[J]. 科学通报, 2015, 60(14): 1298-1309.
本文引用 [1]
[32]
赵俊峰, 刘池洋, 王晓梅, 等. 吕梁山地区中—新生代隆升演化探讨[J]. 地质论评, 2009, 55(5): 663-672.
本文引用 [2]
[33]
赵俊峰, 刘池洋, MOUNTNEY N, 等. 吕梁山隆升时限与演化过程研究[J]. 中国科学: 地球科学, 2015, 45(10): 1427-1438.
本文引用 [2]
[34]
熊保贤, 陈文学, 陈文礼, 等. 巴彦浩特原型盆地形成与演化[J]. 石油实验地质, 2001, 23(1): 19-22, 31.
本文引用 [1]
[35]
黄兴富, 施炜, 李恒强, 等. 银川盆地新生代构造演化: 来自银川盆地主边界断裂运动学的约束[J]. 地学前缘, 2013, 20(4): 199-210.
本文引用 [1]
[36]
付锁堂, 付金华, 喻建, 等. 河套盆地临河坳陷石油地质特征及勘探前景[J]. 石油勘探与开发, 2018, 45(5): 749-762.
本文引用 [1]
[37]
侯光才, 张茂省, 刘方, 等. 鄂尔多斯盆地地下水勘查研究[M]. 北京: 地质出版社, 2008: 1-555.
本文引用 [4]
[38]
WU L Q, JIAO Y Q, ZHU P M, et al. Architectural units and groundwater resource quantity evaluation of Cretaceous sandstones in the Ordos Basin, China[J]. Acta Geologica Sinica(English Edition), 2017, 91(1): 249-262.
本文引用 [2]
[39]
朱强, 司庆红, 李建国, 等. 鄂尔多斯盆地西南部下白垩统洛河组灰色砂岩的两种成因及其含铀性[J]. 地球科学, 2023, 48(11): 3995-4016.
本文引用 [2]
[40]
谢渊, 邓国仕, 刘建清, 等. 鄂尔多斯盆地白垩系主要含水岩组沉积岩相古地理对地下水水化学场形成和水质分布的影响[J]. 沉积与特提斯地质, 2012, 32(3): 64-74.
本文引用 [2]
[41]
刘瑞萍, 李黎, 谢胜凯, 等. LA-HR-ICP-MS小束斑锆石U-Pb年龄和微量元素的同时测定[J]. 世界核地质科学, 2023, 40(2): 435-443.
本文引用 [1]
[42]
GEHRELS G E. Introduction to detrital zircon studies of Paleozoic and Triassic strata in western Nevada and northern California[M]//Geological Society of America special paper 347. Boulder: Geological Society of America, 2000: 1-18.
本文引用 [1]
[43]
HOSKIN P W O, SCHALTEGGER U. The composition of zircon and igneous and metamorphic petrogenesis[J]. Reviews in Mineralogy and Geochemistry, 2003, 53(1): 27-62.
本文引用 [2]
[44]
VERMEESCH P. IsoplotR: a free and open toolbox for geochronology[J]. Geoscience Frontiers, 2018, 9(5): 1479-1493.
本文引用 [1]
[45]
GEHRELS G E, VALENCIA V A, RUIZ J. Enhanced precision, accuracy, efficiency, and spatial resolution of U-Pb ages by laser ablation-multicollector-inductively coupled plasma-mass spectrometry[J]. Geochemistry, Geophysics, Geosystems, 2008, 9(3): Q03017.
本文引用 [1]
[46]
GEHRELS G E, BLAKEY R, KARLSTROM K E, et al. Detrital zircon U-Pb geochronology of Paleozoic strata in the Grand Canyon, Arizona[J]. Lithosphere, 2011, 3(3): 183-200.
本文引用 [1]
[47]
DICKINSON W R. Impact of differential zircon fertility of granitoid basement rocks in North America on age populations of detrital zircons and implications for granite petrogenesis[J]. Earth and Planetary Science Letters, 2008, 275(1/2): 80-92.
本文引用 [1]
[48]
罗红玲, 吴泰然, 李毅. 乌拉特中旗克布岩体的地球化学特征及SHRIMP定年: 早二叠世华北克拉通底侵作用的证据[J]. 岩石学报, 2007, 23(4): 755-766.
本文引用 [3]
[49]
罗红玲, 吴泰然, 赵磊. 华北板块北缘乌梁斯太A型花岗岩体锆石SHRIMP U-Pb定年及构造意义[J]. 岩石学报, 2009, 25(3): 515-526.
本文引用 [3]
[50]
罗红玲, 吴泰然, 赵磊, 等. 白云鄂博中二叠世巴音珠日和岩体地球化学特征及构造意义[J]. 高校地质学报, 2013, 19(1): 123-132.
本文引用 [3]
[51]
LUO H L, WU T R, ZHAO L, et al. Permian high Ba-Sr granitoids: geochemistry, age and tectonic implications of Erlangshan pluton, Urad Zhongqi, Inner Mongolia[J]. Acta Geologica Sinica(English Edition), 2009, 83(3): 603-614.
本文引用 [3]
[52]
ZHANG X H, MAO Q, ZHANG H F, et al. Mafic and felsic magma interaction during the construction of high-K calc-alkaline plutons within a metacratonic passive margin: the Early Permian Guyang batholith from the northern North China Craton[J]. Lithos, 2011, 125(1/2): 569-591.
本文引用 [3]
[53]
张青伟, 刘正宏, 柴社立, 等. 内蒙古乌拉特中旗乌兰地区含石榴石花岗岩锆石U-Pb年龄及地质意义[J]. 吉林大学学报(地球科学版), 2011, 41(3): 745-752.
本文引用 [3]
[54]
董春艳, 万渝生, 徐仲元, 等. 华北克拉通大青山地区古元古代晚期孔兹岩系: 锆石SHRIMP U-Pb定年[J]. 中国科学: 地球科学, 2012, 42(12): 1851-1862.
本文引用 [4]
[55]
MA X D, GUO J H, LIU F, et al. Zircon U-Pb ages, trace elements and Nd-Hf isotopic geochemistry of Guyang sanukitoids and related rocks: implications for the Archean crustal evolution of the Yinshan Block, North China Craton[J]. Precambrian Research, 2013, 230: 61-78.
本文引用 [3]
[56]
DONG C Y, WAN Y S, WILDE S A, et al. Earliest Paleoproterozoic supracrustal rocks in the North China Craton recognized from the Daqingshan area of the khondalite belt: constraints on craton evolution[J]. Gondwana Research, 2014, 25(4): 1535-1553.
本文引用 [3]
[57]
LING M X, ZHANG H, LI H, et al. The Permian-Triassic granitoids in Bayan Obo, North China Craton: a geochemical and geochronological study[J]. Lithos, 2014, 190/191: 430-439.
本文引用 [3]
[58]
ZHANG S H, ZHAO Y, YE H, et al. Origin and evolution of the Bainaimiao arc belt: implications for crustal growth in the southern Central Asian orogenic belt[J]. Geological Society of America Bulletin, 2014, 126(9/10): 1275-1300.
本文引用 [3]
[59]
王梁, 王根厚, 雷时斌, 等. 内蒙古乌拉山大桦背岩体成因: 地球化学、锆石U-Pb年代学及Sr-Nd-Hf同位素制约[J]. 岩石学报, 2015, 31(7): 1977-1994.
本文引用 [3]
[60]
刘平华, 刘福来, 蔡佳, 等. 阴山陆块武川石榴基性麻粒岩P-T条件及其变质时代: 来自相平衡模拟与锆石U-Pb定年的约束[J]. 岩石学报, 2016, 32(7): 1949-1979.
本文引用 [3]
[61]
张琳, 董春艳, 刘守偈, 等. 华北克拉通乌拉山地区早前寒武纪岩浆作用和变质作用: 锆石SHRIMP U-Pb定年及岩石地球化学研究[J]. 地质论评, 2016, 62(6): 1419-1438.
本文引用 [3]
[62]
陈佩嘉, 戴朝成, 黄成, 等. 乌拉山地区古元古代S型花岗岩岩石地球化学、锆石U-Pb年代学及其地质意义[J]. 中国地质, 2017, 44(5): 959-973.
本文引用 [3]
[63]
李长海, 刘正宏, 赵庆英, 等. 内蒙古商都地区白云鄂博群尖山组碎屑锆石U-Pb年代学和Hf同位素研究: 对华北克拉通西部陆块北缘前寒武纪地壳演化的制约[J]. 岩石学报, 2020, 36(9): 2815-2833.
本文引用 [3]
[64]
彭润民, 翟裕生, 王建平, 等. 内蒙狼山新元古代酸性火山岩的发现及其地质意义[J]. 科学通报, 2010, 55(26): 2611-2620.
本文引用 [3]
[65]
孙立新, 赵凤清, 王惠初, 等. 内蒙古狼山地区宝音图地块变质基底的锆石U-Pb年龄及构造意义[J]. 地质学报, 2013, 87(2): 197-207.
本文引用 [3]
[66]
吴亚飞, 曾键年, 曹建劲, 等. 内蒙古东升庙海西期岩体锆石U-Pb年龄及Hf同位素特征[J]. 地质科技情报, 2013, 32(6): 22-30.
本文引用 [3]
[67]
LIN L, XIAO W, WAN B, et al. Geochronologic and geochemical evidence for persistence of south-dipping subduction to Late Permian time, Langshan area, Inner Mongolia (China): significance for termination of accretionary orogenesis in the southern Altaids[J]. American Journal of Science, 2014, 314(2): 679-703.
本文引用 [3]
[68]
HU C S, LI W B, XU C, et al. Geochemistry and petrogenesis of Permian granitoids in the northwestern margin of the North China Craton: insights from the Dongshengmiao pluton, Inner Mongolia[J]. International Geology Review, 2015, 57(14): 1843-1860.
本文引用 [3]
[69]
WAN B, WINDLEY B F, XIAO W J, et al. Paleoproterozoic high-pressure metamorphism in the northern North China Craton and implications for the Nuna supercontinent[J]. Nature Communications, 2015, 6: 8344.
本文引用 [3]
[70]
WANG Z Z, HAN B F, FENG L X, et al. Geochronology, geochemistry and origins of the Paleozoic-Triassic plutons in the Langshan area, western Inner Mongolia, China[J]. Journal of Asian Earth Sciences, 2015, 97: 337-351.
本文引用 [3]
[71]
WANG Z Z, HAN B F, FENG L X, et al. Tectonic attribution of the Langshan area in western Inner Mongolia and implications for the Neoarchean-Paleoproterozoic evolution of the Western North China Craton: evidence from LA-ICP-MS zircon U-Pb dating of the Langshan basement[J]. Lithos, 2016, 261: 278-295.
本文引用 [3]
[72]
DAN W, LI X H, WANG Q, et al. Phanerozoic amalgamation of the Alxa Block and North China Craton: evidence from Paleozoic granitoids, U-Pb geochronology and Sr-Nd-Pb-Hf-O isotope geochemistry[J]. Gondwana Research, 2016, 32: 105-121.
本文引用 [4]
[73]
LIU C H, ZHAO G C, LIU F L, et al. Late Precambrian tectonic affinity of the Alxa Block and the North China Craton: evidence from zircon U-Pb dating and Lu-Hf isotopes of the Langshan Group[J]. Precambrian Research, 2019, 326: 312-332.
本文引用 [3]
[74]
DONG C Y, LIU D Y, LI J J, et al. Palaeoproterozoic khondalite belt in the western North China Craton: new evidence from SHRIMP dating and Hf isotope composition of zircons from metamorphic rocks in the Bayan Ul-Helan Mountains Area[J]. Chinese Science Bulletin, 2007, 52(21): 2984-2994.
本文引用 [3]
[75]
耿元生, 周喜文. 阿拉善地区新元古代岩浆事件及其地质意义[J]. 岩石矿物学杂志, 2010, 29(6): 779-795.
本文引用 [3]
[76]
耿元生, 周喜文. 阿拉善地区新元古代早期花岗岩的地球化学和锆石Hf同位素特征[J]. 岩石学报, 2011, 27(4): 897-908.
本文引用 [3]
[77]
耿元生, 周喜文. 阿拉善变质基底中的早二叠世岩浆热事件: 来自同位素年代学的证据[J]. 岩石学报, 2012, 28(9): 2667-2685.
本文引用 [3]
[78]
DAN W, LI X H, GUO J H, et al. Integrated in situ zircon U-Pb age and Hf-O isotopes for the Helanshan khondalites in North China Craton: juvenile crustal materials deposited in active or passive continental margin?[J]. Precambrian Research, 2012, 222/223: 143-158.
本文引用 [3]
[79]
DAN W, LI X H, GUO J H, et al. Paleoproterozoic evolution of the eastern Alxa Block, westernmost North China: evidence from in situ zircon U-Pb dating and Hf-O isotopes[J]. Gondwana Research, 2012, 21(4): 838-864.
本文引用 [3]
[80]
DAN W, LI X H, WANG Q, et al. An Early Permian (ca. 280 Ma) silicic igneous province in the Alxa Block, NW China: a magmatic flare-up triggered by a mantle-plume?[J]. Lithos, 2014, 204: 144-158.
本文引用 [3]
[81]
DAN W, LI X H, WANG Q, et al. Neoproterozoic S-type granites in the Alxa Block, westernmost North China and tectonic implications: in situ zircon U-Pb-Hf-O isotopic and geochemical constraints[J]. American Journal of Science, 2014, 314(1): 110-153.
本文引用 [3]
[82]
DAN W, WANG Q, WANG X C, et al. Overlapping Sr-Nd-Hf-O isotopic compositions in Permian mafic enclaves and host granitoids in Alxa Block, NW China: evidence for crust-mantle interaction and implications for the generation of silicic igneous provinces[J]. Lithos, 2015, 230: 133-145.
本文引用 [3]
[83]
史兴俊, 童英, 王涛, 等. 内蒙古西部阿拉善地区哈里努登花岗岩LA-ICP-MS锆石U-Pb年龄和地球化学特征[J]. 地质通报, 2012, 31(5): 662-670.
本文引用 [3]
[84]
ZHANG J, LI J Y, XIAO W X, et al. Kinematics and geochronology of multistage ductile deformation along the eastern Alxa Block, NW China: new constraints on the relationship between the North China Plate and the Alxa Block[J]. Journal of Structural Geology, 2013, 57: 38-57.
本文引用 [3]
[85]
SHI X J, WANG T, ZHANG L, et al. Timing, petrogenesis and tectonic setting of the Late Paleozoic gabbro-granodiorite-granite intrusions in the Shalazhashan of northern Alxa: constraints on the southernmost boundary of the Central Asian Orogenic Belt[J]. Lithos, 2014, 208/209: 158-177.
本文引用 [3]
[86]
WU S J, HU J M, REN M H, et al. Petrography and zircon U-Pb isotopic study of the Bayanwulashan Complex: constraints on the Paleoproterozoic evolution of the Alxa Block, westernmost North China Craton[J]. Journal of Asian Earth Sciences, 2014, 94: 226-239.
本文引用 [3]
[87]
LIU Q, ZHAO G C, SUN M, et al. Early Paleozoic subduction processes of the Paleo-Asian Ocean: insights from geochronology and geochemistry of Paleozoic plutons in the Alxa Terrane[J]. Lithos, 2016, 262: 546-560.
本文引用 [3]
[88]
DARBY B J, GEHRELS G. Detrital zircon reference for the North China Block[J]. Journal of Asian Earth Sciences, 2006, 26(6): 637-648.
本文引用 [3]
[89]
YIN C Q, ZHAO G C, SUN M, et al. LA-ICP-MS U-Pb zircon ages of the Qianlishan Complex: constraints on the evolution of the khondalite belt in the western block of the North China Craton[J]. Precambrian Research, 2009, 174(1/2): 78-94.
本文引用 [3]
[90]
张进, 李锦轶, 刘建峰, 等. 早古生代阿拉善地块与华北地块之间的关系: 来自阿拉善东缘中奥陶统碎屑锆石的信息[J]. 岩石学报, 2012, 28(9): 2912-2934.
本文引用 [3]
[91]
李黎明, 曾佐勋, 陆彦俊, 等. 孔兹岩系: 贺兰山中段赵池沟岩组碎屑锆石LA-ICP-MS锆石U-Pb年代学、Hf同位素组成及其地质意义[J]. 科学通报, 2014, 59(7): 593-608.
本文引用 [3]
[92]
SHI G Z, SOARES C J, SHEN C B, et al. Combined detrital zircon fission track and U-Pb dating of the Late Paleozoic to Early Mesozoic sandstones in the Helanshan, western Ordos fold-thrust belt: constraints for provenance and exhumation history[J]. Journal of Geodynamics, 2019, 130: 57-71.
本文引用 [3]
[93]
SUN J P, DONG Y P. Middle-Late Triassic sedimentation in the Helanshan tectonic belt: constraints on the tectono-sedimentary evolution of the Ordos Basin, North China[J]. Geoscience Frontiers, 2019, 10(1): 213-227.
本文引用 [3]
[94]
PANG L Y, ZHU X Y, HU B, et al. Detrital zircon U-Pb age and Hf isotopic composition and whole-rock geochemical characteristics of the Statherian Huangqikou Formation, western margin of the North China Craton: implications for provenance and tectonic evolution[J]. Precambrian Research, 2020, 347: 105840.
本文引用 [3]
[95]
ZHANG T R, MYROW P M, FIKE D A, et al. Sedimentology, stratigraphy, and detrital zircon geochronology of Mesoproterozoic strata in the northern Helan Mountains, western margin of the North China Block[J]. Precambrian Research, 2020, 343: 105730.
本文引用 [3]
[96]
乔恒忠. 华北西部千里山地区长城系黄旗口组碎屑锆石U-Pb年龄及其地质意义[J]. 四川地质学报, 2021, 41(1): 33-39, 56.
本文引用 [3]
[97]
ZHAO G C, WILDE S A, GUO J H, et al. Single zircon grains record two Paleoproterozoic collisional events in the North China Craton[J]. Precambrian Research, 2010, 177(3/4): 266-276.
本文引用 [1]
[98]
蔡佳, 刘福来, 刘平华, 等. 内蒙古孔兹岩带乌拉山—大青山地区古元古代孔兹岩系年代学研究[J]. 岩石学报, 2015, 31(10): 3081-3106.
本文引用 [1]
[99]
卓鱼周. 鄂尔多斯盆地西北部桌子山地区中—新生代隆升事件的确定及其构造意义[D]. 西安: 西北大学, 2015.
本文引用 [1]
[100]
马静辉, 何登发, 开百泽, 等. 贺兰山构造带构造-地层层序及构造演化[J]. 地质科学, 2020, 55(3): 852-876.
本文引用 [1]
[101]
JOLIVET M, BRAUCHER R, DOVCHINTSEREN D, et al. Erosion around a large-scale topographic high in a semi-arid sedimentary basin: interactions between fluvial erosion, aeolian erosion and aeolian transport[J]. Geomorphology, 2021, 386: 107747.
本文引用 [1]
[102]
ZHAO H L, AO C, LI J G, et al. Occurrence and mechanism of uranium enrichment with a unique eolian sedimental environment in the Pengyang uranium deposit, Ordos Basin[J]. Ore Geology Reviews, 2022, 141: 104641.
本文引用 [1]

基金

中核集团集中研发项目(中核科发2021-143号)
中国铀业有限公司-东华理工大学核资源与环境国家重点实验室联合创新基金项目(2022NRE-LH-16)
中核集团青年英才项目(地QNYC2301)

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