Volume 32 Issue 4
Aug.  2026
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Article Navigation >  Journal of Geomechanics  > 2026  >  32(4): 942-957
SHI Z Q，SUN L，ZHANG H，et al.，2026. Tectonic evolution of the western Yangtze Block during the Ediacaran–Cambrian: evidence from detrital zircon U-Pb geochronology[J]. Journal of Geomechanics，32（4）：942−957 doi: 10.12090/j.issn.1006-6616.2025065
Citation: SHI Z Q，SUN L，ZHANG H，et al.，2026. Tectonic evolution of the western Yangtze Block during the Ediacaran–Cambrian: evidence from detrital zircon U-Pb geochronology[J]. Journal of Geomechanics，32（4）：942−957 doi: 10.12090/j.issn.1006-6616.2025065
shu

Tectonic evolution of the western Yangtze Block during the Ediacaran–Cambrian: evidence from detrital zircon U-Pb geochronology

doi: 10.12090/j.issn.1006-6616.2025065
  • 1.

    Third Geological Exploration Institute, China Metallurgical Geology Bureau, Taiyuan 030000, Shanxi, China

  • 2.

    Kunming Geological Exploration Institute, China Metallurgical Geology Bureau, Kunming 650000, Yunnan, China

Funds:  This research was financially supported by the Geological Comprehensive Research Project of the China Metallurgical Geology Bureau (Grant No.[2025] CMGBDZYJ003).
More Information
  • Received: 2025-06-10
  • Revised: 2026-04-02
  • Accepted: 2026-04-02
    • Available Online: 2026-04-02
  • Published: 2026-08-28
    Abstract
  •   Objective  The Yangtze Block was a crucial component of the Gondwana supercontinent. During the Ediacaran–Early Cambrian, its western margin underwent a marked transition from carbonate- to siliciclastic-dominated depositional environments. However, the tectonic dynamics and geotectonic setting governing this pronounced sedimentary facies shift remain poorly constrained. Thick Lower Cambrian terrigenous clastic rocks widely exposed along the western margin of the Yangtze Block (Western Yangtze) serve as a key archive for tracing sediment provenance and deciphering Early Cambrian geotectonic evolution.  Methods  This study presents systematic detrital zircon U–Pb geochronological and whole-rock major- and trace-element geochemical analyses of the Lower Cambrian Qiongzhusi Formation in the Western Yangtze to constrain its provenance and tectonic background.  Results  Whole-rock geochemical data indicate that high-field-strength elements (HFSEs) and large-ion lithophile elements (LILEs; e.g., Th, Zr, Hf, Ba, Pb) in the Qiongzhusi Formation clastic rocks align closely with upper continental crust (UCC) values. Conversely, elements such as Co, Ni, Y, Nb, Cs, Hf, and Ta are depleted relative to UCC, with Co, Cs, and Ta showing the most significant depletion. Characteristics of immobile elements (Th, Sc, Hf, Zr, Ho) and rare earth elements (REEs; e.g., La, Ce, Yb) consistently indicate a predominantly felsic igneous source. Detrital zircon U–Pb age spectra exhibit two primary population peaks at ca. 590–500 Ma and ca. 880–720 Ma, alongside two subordinate clusters at ca. 1900–1500 Ma and ca. 2500–2400 Ma.  Conclusions  Integrated with regional geological evidence, we propose that the Early Cambrian detritus was primarily derived from Ediacaran–Early Cambrian magmatic rocks within the Longmenshan tectonic belt, as well as weathering products of late Neoproterozoic felsic magmatic rocks from the Panxi–Hannan and Ailaoshan magmatic arcs. Subduction of the Proto-Tethys Ocean beneath the Western Yangtze during the latest Ediacaran–Early Cambrian established a Late Ediacaran–Early Cambrian magmatic arc. This tectonic event converted the Western Yangtze from a passive margin into an active continental margin, supplying voluminous Early Cambrian detritus that drove the major depositional transition from carbonates to siliciclastics. [ Significance ]These findings establish key provenance links between the Western Yangtze and surrounding orogenic belts, providing critical constraints for reconstructing the tectonic and paleogeographic evolution of the South China Block during the Ediacaran–Early Cambrian transition.

     

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    • References(97)
  • [1]
    ANDERSEN T, 2002. Correction of common lead in U-Pb analyses that do not report 204Pb. Chemical Geology, 192(1–2): 59–79.
    [2]
    BHATIA M R, 1983. Plate tectonics and geochemical composition of sandstones[J]. The Journal of Geology, 91(6): 611-627. doi: 10.1086/628815
    [3]
    BHATIA M R, CROOK K A W, 1986. Trace element characteristics of graywackes and tectonic setting discrimination of sedimentary basins[J]. Contributions to Mineralogy and Petrology, 92(2): 181-193. doi: 10.1007/BF00375292
    [4]
    Bureau of Geology and Mineral Resources of Yunnan Province. 1990. Regional Geology of Yunnan Province[M]. Beijing: Geological Publishing House.
    [5]
    CAI Y F, WANG Y J, CAWOOD P A, et al., 2014. Neoproterozoic subduction along the Ailaoshan zone, South China: geochronological and geochemical evidence from amphibolite[J]. Precambrian Research, 245: 13-28. doi: 10.1016/j.precamres.2014.01.009
    [6]
    CAI Y F, WANG Y J, CAWOOD P A, et al., 2015. Neoproterozoic crustal growth of the Southern Yangtze Block: geochemical and zircon U-Pb geochronological and Lu-Hf isotopic evidence of Neoproterozoic diorite from the Ailaoshan zone[J]. Precambrian Research, 266: 137-149. doi: 10.1016/j.precamres.2015.05.008
    [7]
    CAWOOD P A, HAWKESWORTH C J, DHUIME B, 2012. Detrital zircon record and tectonic setting[J]. Geology, 40(10): 875-878. doi: 10.1130/G32945.1
    [8]
    CHEN Q, SUN M, LONG X P, et al., 2016. U-Pb ages and Hf isotopic record of zircons from the Late Neoproterozoic and Silurian-Devonian sedimentary rocks of the western Yangtze Block: implications for its tectonic evolution and continental affinity[J]. Gondwana Research, 31: 184-199. doi: 10.1016/j.gr.2015.01.009
    [9]
    CHEN Q, ZHAO G C, SUN M, 2021. Protracted northward drifting of South China during the assembly of Gondwana: constraints from the spatial-temporal provenance comparison of Neoproterozoic-Cambrian strata[J]. GSA Bulletin, 133(9-10): 1947-1963. doi: 10.1130/B35791.1
    [10]
    CHEN S D, XU Z Q, SONG H, et al., 2023. Geochemical characteristics and sedimentary environment of Qiongzhusi Formation in Daibuzhen, Huize Area, Yunnan Province[J]. Sichuan Metallurgy, 45(1): 12-21. (in Chinese with English abstract)
    [11]
    DENG Q, WANG Z J, LIU H, et al., 2025. Subduction-collision and rapid uplift of the NW Yangtze Block during the Ediacaran-Cambrian transition: new evidence from the shoshonite series[J]. International Geology Review, 67(3): 331-351. doi: 10.1080/00206814.2024.2446942
    [12]
    DENG T L, PENG Y W, CHENG W B, et al., 2025. Geochronology, petrogenesis, and tin-tungsten metallogenic potential of the Neoproterozoic highly fractionated granites in the Mosuoying area, western margin of the Yangtze Block[J]. Journal of Chengdu University of Technology (Science & Technology Edition), 52(3): 456-479. (in Chinese with English abstract)
    [13]
    FENG Z Z, PENG Y M, JIN Z K, et al., 2001. Lithofacies palaeogeography of the Cambrian in South China[J]. Journal of Palaeogeography, 3(1): 1-14. (in Chinese with English abstract)
    [14]
    FENG Z Z, PENG Y M, JIN Z K, et al., 2002. Lithofacies palaeogeography of the Early Cambrian in China[J]. Journal of Palaeogeography, 4(1): 1-12. (in Chinese with English abstract)
    [15]
    FLOYD P A, LEVERIDGE B E, 1987. Tectonic environment of the Devonian Gramscatho basin, south Cornwall: framework mode and geochemical evidence from turbiditic sandstones[J]. Journal of the Geological Society, 144(4): 531-542. doi: 10.1144/gsjgs.144.4.0531
    [16]
    GEHRELS G E, DECELLES P G, OJHA T P, et al., 2006. Geologic and U-Pb geochronologic evidence for Early Paleozoic tectonism in the Dadeldhura thrust sheet, far-west Nepal Himalaya[J]. Journal of Asian Earth Sciences, 28(4-6): 385-408. doi: 10.1016/j.jseaes.2005.09.012
    [17]
    GRIMES C B, JOHN B E, KELEMEN P B, et al., 2007. Trace element chemistry of zircons from oceanic crust: a method for distinguishing detrital zircon provenance[J]. Geology, 35(7): 643-646. doi: 10.1130/G23603A.1
    [18]
    GU Z D, LONERGAN L, ZHAI X F, et al., 2021. The formation of the Sichuan Basin, South China, during the Late Ediacaran to Early Cambrian[J]. Basin Research, 33(4): 2328-2357. doi: 10.1111/bre.12559
    [19]
    GU Z D, JIAN X, WATTS A B, et al., 2023. Formation and evolution of an Early Cambrian foreland basin in the NW Yangtze Block, South China[J]. Journal of the Geological Society, 180(3): jgs2022-127. doi: 10.5194/egusphere-egu24-9027
    [20]
    HE W H, TANG T T, YUE M L, et al., 2014. Sedimentary and tectonic evolution of Nanhuan-Permian in South China[J]. Earth Science—Journal of China University of Geosciences, 39(8): 929-953. (in Chinese with English abstract)
    [21]
    JIANG G Q, SOHL L E, CHRISTIE-BLICK N, 2003. Neoproterozoic stratigraphic comparison of the Lesser Himalaya (India) and Yangtze block (South China): paleogeographic implications[J]. Geology, 31(10): 917-920. doi: 10.1130/G19790.1
    [22]
    JIANG G Q, SHI X Y, ZHANG S H, et al., 2011. Stratigraphy and paleogeography of the Ediacaran Doushantuo Formation (ca. 635-551 Ma) in South China[J]. Gondwana Research, 19(4): 831-849. doi: 10.1016/j.gr.2011.01.006
    [23]
    LI L M, LIN S F, XING G F, et al., 2017. First direct evidence of Pan-African orogeny associated with Gondwana assembly in the Cathaysia block of southern China[J]. Scientific Reports, 7(1): 794. doi: 10.1038/s41598-017-00950-x
    [24]
    LI Y B, REN X, SAFONOVA I, et al., 2025. Early Neoproterozoic oceanic subduction along the western Yangtze Block: constraints from the genesis of Tianquan diorites in the western Sichuan[J]. Journal of Chengdu University of Technology (Science & Technology Edition), 52(3): 480-501. (in Chinese with English abstract)
    [25]
    LIN S F, WANG L J, XIAO W J, et al. , 2024. The Early Paleozoic Wuyi-Yunkai orogeny in South China: a collisional orogeny with a major lag in time between onset of collision and peak metamorphism in subducted continental crust[M]//NANCE R D, STRACHAN R A, QUESADA C, et al. Supercontinents, orogenesis and magmatism. London: Geological Society, London, Special Publications: 649-641.
    [26]
    LIU B B, PENG T P, FAN W M, et al., 2020. Tectonic evolution and paleoposition of the Baoshan and Lincang blocks of West Yunnan during the Paleozoic[J]. Tectonics, 39(10): e2019TC006028. doi: 10.1029/2019TC006028
    [27]
    LIU B B, PENG T P, FAN W M, et al., 2023. Correlation between South China and India and development of double rift systems in the South China-India Duo during late Neoproterozoic time[J]. GSA Bulletin, 135(1-2): 351-366. doi: 10.1130/B36397.1
    [28]
    LIU B B, YAN Q H, SHI Z Q, et al., 2025. Late Neoproterozoic-Middle Cambrian tectonic affinity and paleogeographic position of the South China Block and its geotectonic significance[J]. Geotectonica et Metallogenia, 49(4): 975-988. (in Chinese with English abstract)
    [29]
    LIU H P, RONG J, LIU Z L, et al., 2025. Element geochemical characteristics and geological significance of the Cambrian Qiongzhusi Formation in northern Guangyuan, Sichuan Basin[J]. Natural Gas Geoscience, 36(5): 936-952. (in Chinese with English abstract)
    [30]
    LIU X Y, CAO J, LI S S, et al., 2023. Geochemical characteristics and geological significance of Neoproterozoic Qingmingshan granite in northern Guangxi[J]. Journal of Guilin University of Technology, 43(3): 351-363. (in Chinese with English abstract)
    [31]
    LIU Y S, HU Z C, ZONG K Q, et al., 2010. Reappraisement and refinement of zircon U-Pb isotope and trace element analyses by LA-ICP-MS[J]. Chinese Science Bulletin, 55(15): 1535-1546. doi: 10.1007/s11434-010-3052-4
    [32]
    LUDWIG K R, 2003. User's manual for Isoplot 3.00: a geochronological toolkit for Microsoft Excel[M]. Berkeley: Berkeley Geochronology Center.
    [33]
    MCDONOUGH W F, SUN S S, 1995. The composition of the Earth[J]. Chemical Geology, 120(3-4): 223-253. doi: 10.1016/0009-2541(94)00140-4
    [34]
    MCLENNAN S M, 1989. Rare earth elements in sedimentary rocks: influence of provenance and sedimentary processes. Rev. Mineral. 21: 169–200.
    [35]
    MCLENNAN S M, HEMMING S, MCDANIEL D K, et al. , 1993. Geochemical approaches to sedimentation, provenance, and tectonics[M]//JOHNSSON M J, BASU A. Processes controlling the composition of clastic sediments. Geological Society of America: 21-40.
    [36]
    MORADI A, SHABANIAN N, DAVOUDIAN A R, et al., 2022. Zircon U-Pb and geochemistry of the north Shahrekord metamorphosed felsic rocks: implications for the Ediacaran-Cambrian tectonic setting of Iran[J]. International Journal of Earth Sciences, 111(7): 2239-2263. doi: 10.1007/s00531-022-02225-x
    [37]
    QI L, XU Y J, DU Y S, et al., 2023. Neoproterozoic sedimentary records in the Cathaysia Block and their implications for the supercontinent reconstruction[J]. Sedimentary Geology and Tethyan Geology, 43(1): 188-211. (in Chinese with English abstract)
    [38]
    RUDNICK R L, GAO S, 2014. Composition of the continental crust[M]//HOLLAND H D, TUREKIAN K K. Treatise on geochemistry. Oxford: Elsevier: 1-51.
    [39]
    SHAFAII MOGHADAM H, GRIFFIN W L, LI X H, et al., 2017. Crustal evolution of NW Iran: Cadomian arcs, Archean fragments and the Cenozoic magmatic flare-up[J]. Journal of Petrology, 58(11): 2143-2190. doi: 10.1093/petrology/egy005
    [40]
    SHAHZEIDI M, MOAYYED M, MURATA M, et al., 2017. Late Ediacaran crustal thickening in Iran: geochemical and isotopic constraints from the ~550 Ma Mishu granitoids (northwest Iran)[J]. International Geology Review, 59(7): 793-811. doi: 10.1080/00206814.2016.1198728
    [41]
    SONG H, XU Z Q, NI S J, et al., 2015. Response of the motianling granitic pluton in North Guangxi to the tectonic evolution in the southwestern section of the Jiangnan Orogenic Belt: constraints from neoproterozoic zircon geochronology[J]. Geotectonica et Metallogenia, 39(6): 1156-1175. (in Chinese with English abstract)
    [42]
    TAYLOR S R, MCLENNAN S M, 1985. The continental crust: its composition and evolution[M]. Oxford: Blackwell Scientific Publications.
    [43]
    TIAN Z D, LENG C B, and ZHANG, X C, 2020. Provenance and tectonic setting of the Neoproterozoic metasedimentary rocks at southeastern Tibetan Plateau: Implications for the tectonic affinity of Yidun terrane: Precambrian Research, 344: 1–19,
    [44]
    VERMEESCH P, 2012. On the visualisation of detrital age distributions[J]. Chemical Geology, 312-313: 190-194.
    [45]
    WANG J, LI Z X, 2003. History of Neoproterozoic rift basins in South China: implications for Rodinia break-up[J]. Precambrian Research, 122(1-4): 141-158. doi: 10.1016/s0301-9268(02)00209-7
    [46]
    WANG L J, YU J H, GRIFFIN W L, et al. , 2012. Early crustal evolution in the western Yangtze Block: evidence from U-Pb and Lu-Hf isotopes on detrital zircons from sedimentary rocks[J]. Precambrian Research, 222-223: 368-385.
    [47]
    WANG L J, LIN S F, XIAO W J, 2023. Yangtze and Cathaysia blocks of South China: their separate positions in Gondwana until early Paleozoic juxtaposition[J]. Geology, 51(8): 723-727. doi: 10.1130/geol.s.23060891.v1
    [48]
    WANG S D, DUAN X X, CAI X B, et al., 2023. Enrichment and fractionation of REY in the weathering crust of metamorphic rocks in the Shiguan Area of the Dabie Orogenic Belt[J]. Geology and Exploration, 59(4): 828-851. (in Chinese with English abstract)
    [49]
    WANG Y P, BAO Z D, ZHANG L J, et al., 2024. Diagenesis of microbial dolomite reservoirs in the second Member of Dengying Formation of Ediacaran in the Penglai area, Sichuan Basin: Insights into the formation and evolution of high-quality reservoirs[J]. Journal of Geomechanics, 30(4): 579-594. (in Chinese with English abstract)
    [50]
    WRONKIEWICZ D J, CONDIE K C, 1987. Geochemistry of Archean shales from the Witwatersrand Supergroup, South Africa: source-area weathering and provenance[J]. Geochimica et Cosmochimica Acta, 51(9): 2401-2416. doi: 10.1016/0016-7037(87)90293-6
    [51]
    WU Y B, ZHENG Y F, 2004. Genesis of zircon and its constraints on interpretation of U-Pb age[J]. Chinese Science Bulletin, 49(15): 1554-1569. doi: 10.1007/BF03184122
    [52]
    XIA X P, NIE X S, LAI C K, et al., 2016. Where was the Ailaoshan Ocean and when did it open: a perspective based on detrital zircon U-Pb age and Hf isotope evidence[J]. Gondwana Research, 36: 488-502. doi: 10.1016/j.gr.2015.08.006
    [53]
    XIONG J Y, ZHANG Z B, LIU S R, 1980. The eighth team of Regional Geological Investigation Team, Geological Bureau of Yunnan Province. Regional Geological Survey Report of the People's Republic of China 1: 200000 Dongchuan G-48-XIV[R]. Yuxi: Geological Bureau of Yunnan Province (In Chinese).
    [54]
    XU Y F, 2018. The Definition of the Paleoproterozoic Stratum and the prospecting significance in the Yimen area, central Yunnan Province[D]. Kunming: Kunming University of Science and Technology. (in Chinese with English abstract)
    [55]
    YANG C, LI X H, LI Z X, et al., 2020. Provenance evolution of age-calibrated strata reveals when and how South China Block collided with Gondwana[J]. Geophysical Research Letters, 47(19): e2020GL090282. doi: 10.1029/2020GL090282
    [56]
    YANG J H, CAWOOD P A, DU Y S, et al. , 2012. Large igneous province and magmatic arc sourced Permian-Triassic volcanogenic sediments in China[J]. Sedimentary Geology, 261-262: 120-131.
    [57]
    YANG Y Z, GUO L, FANG Z X, et al., 2024. Weathering characteristics of sedimentary source area of Qiongzhusi Formation, eastern margin of Ancient Kangding-Yunnan Land: case study of the Wulongcun section of Wuding district, Chuxiong City, Yunnan province, China[J]. Acta Sedimentologica Sinica, 42(1): 324-341. (in Chinese with English abstract)
    [58]
    YAO J L, CAWOOD P A, SHU L S, et al., 2019. Jiangnan Orogen, South China: a~970-820 Ma Rodinia margin accretionary belt[J]. Earth-Science Reviews, 196: 102872. doi: 10.1016/j.earscirev.2019.05.016
    [59]
    ZHAN S W, 2023. Geochemical characteristics and geological significance of Lugu granite in the western margin of the Yangtze Block[D]. Chengdu: Chengdu University of Technology. (in Chinese with English abstract)
    [60]
    ZHANG D M, CHENG X, WEI B T, et al., 2023. Magnetic fabric study of the Cambrian Stage 3 sedimentary rocks in Eastern Yunnan and its implications for paleocurrent direction[J]. Journal of Northwest University (Natural Science Edition), 53(4): 655-670. (in Chinese with English abstract)
    [61]
    ZHANG K X, PAN G T, HE W H, et al., 2015. New division of tectonic-strata superregion in China[J]. Earth Science—Journal of China University of Geosciences, 40(2): 206-233. (in Chinese with English abstract)
    [62]
    ZHANG K X, HE W H, XU Y D, et al., 2023. The division of Qingbaikouan-Triassic tectono-stratigraphic regions and their characteristics in South China[J]. South China Geology, 39(1): 1-23. (in Chinese with English abstract)
    [63]
    ZHANG S, LUO B, WANG Z C, et al., 2025. Genesis of the Deyang-Anyue intracratonic rift in the Sichuan Basin and its connection with the Proto-Tethys Ocean[J]. Natural Gas Industry, 45(2): 37-50. (in Chinese with English abstract)
    [64]
    ZHANG Y L, JIA X T, WANG Z Q, et al., 2018. New insights into provenance of Early Cambrian Xiannüdong Formation in the Micangshan Area: evidence from sedimentology, heavy mineral and detrital zircon chronology[J]. Acta Geologica Sinica, 92(9): 1918-1935. (in Chinese with English abstract)
    [65]
    ZHAO G C, WANG Y J, HUANG B C, et al., 2018. Geological reconstructions of the East Asian blocks: from the breakup of Rodinia to the assembly of Pangea[J]. Earth-Science Reviews, 186: 262-286. doi: 10.1016/j.earscirev.2018.10.003
    [66]
    ZHAO G C, HAN Y G, LI J H, et al., 2022. Environmental effects of assembly and breakup of supercontinents[J]. Acta Geologica Sinica, 96(9): 3120-3127. (in Chinese with English abstract)
    [67]
    ZHAO J H, ASIMOW P D, ZHOU M F, et al., 2017. An Andean-type arc system in Rodinia constrained by the Neoproterozoic Shimian ophiolite in South China[J]. Precambrian Research, 296: 93-111. doi: 10.1016/j.precamres.2017.04.017
    [68]
    ZHAO J H, NEBEL O, JOHNSON T E, 2021. Formation and evolution of a Neoproterozoic continental magmatic arc[J]. Journal of Petrology, 62(8): egab029. doi: 10.1093/petrology/egab029
    [69]
    ZHAO T Y, CAWOOD P A, ZI J W, et al., 2019. Early Paleoproterozoic magmatism in the Yangtze Block: evidence from zircon U-Pb ages, Sr-Nd-Hf isotopes and geochemistry of ca. 2.3 Ga and 2.1 Ga granitic rocks in the Phan Si Pan Complex, north Vietnam[J]. Precambrian Research, 324: 253-268. doi: 10.1016/j.precamres.2019.01.012
    [70]
    ZHOU M Z, LUO T Y, HUANG Z L, et al., 2011. Early Cambrian volcanic records in Guizhou Province, China and their geological significances[J]. Acta Mineralogica Sinica, 31(3): 453-461. (in Chinese with English abstract)
    [71]
    ZHOU M Z, LUO T Y, HUFF W D, et al., 2018. Timing the termination of the Doushantuo negative carbon isotope excursion: evidence from U-Pb ages from the Dengying and Liuchapo formations, South China[J]. Science Bulletin, 63(21): 1431-1438. doi: 10.1016/j.scib.2018.10.002
    [72]
    陈思达, 徐争启, 宋昊, 等, 2023. 云南省会泽地区待补镇筇竹寺组岩石地球化学特征及沉积环境分析[J]. 四川冶金, 45(1): 12-21. doi: 10.3969/j.issn.1001-5108.2023.01.004
    [73]
    邓藤丽, 彭义伟, 程文斌, 等, 2025. 扬子西缘摩挲营新元古代高分异花岗岩年龄、成因和锡钨成矿潜力[J]. 成都理工大学学报(自然科学版), 52(3): 456-479. doi: 10.12474/cdlgzrkx.2024112601
    [74]
    冯增昭, 彭勇民, 金振奎, 等, 2001. 中国南方寒武纪岩相古地理[J]. 古地理学报, 3(1): 1-14. doi: 10.3969/j.issn.1671-1505.2001.01.001
    [75]
    冯增昭, 彭勇民, 金振奎, 等, 2002. 中国早寒武世岩相古地理[J]. 古地理学报, 4(1): 1-12. doi: 10.3969/j.issn.1671-1505.2002.01.001
    [76]
    何卫红, 唐婷婷, 乐明亮, 等, 2014. 华南南华纪-二叠纪沉积大地构造演化[J]. 地球科学—中国地质大学学报, 39(8): 929-953. doi: 10.3799/dqkx.2014.087
    [77]
    李亚博, 任祥, SAFONOVA I, 等, 2025. 扬子西缘新元古代早期大洋俯冲作用: 来自川西天全闪长岩成因的制约[J]. 成都理工大学学报(自然科学版), 52(3): 480-501. doi: 10.12474/cdlgzrkx.2025021002
    [78]
    刘兵兵, 闫庆贺, 史志强, 等, 2025. 华南板块新元古代晚期-中寒武世古地理格局及其大地构造意义[J]. 大地构造与成矿学, 49(4): 975-988. doi: 10.16539/j.ddgzyckx.2024.01.157
    [79]
    刘慧萍, 戎佳, 刘自亮, 等, 2025. 四川盆地广元北部寒武系筇竹寺组元素地球化学特征及地质意义[J]. 天然气地球科学, 36(5): 936-952. doi: 10.11764/j.issn.1672-1926.2024.10.008
    [80]
    刘兴源, 曹杰, 李赛赛, 等, 2023. 桂北新元古代清明山花岗岩地球化学特征及其地质意义[J]. 桂林理工大学学报, 43(3): 351-363. doi: 10.3969/j.issn.1674-9057.2023.03.001
    [81]
    齐靓, 徐亚军, 杜远生, 等, 2023. 华夏地块新元古代沉积记录与超大陆重建[J]. 沉积与特提斯地质, 43(1): 188-211. doi: 10.3969/j.issn.1009-3850.2023.01.015
    [82]
    宋昊, 徐争启, 倪师军, 等, 2015. 广西摩天岭岩体对江南造山带西南段构造演化的响应: 来自新元古代花岗岩锆石U-Pb年代学证据[J]. 大地构造与成矿学, 39(6): 1156-1175. doi: 10.16539/j.ddgzyckx.2015.06.015
    [83]
    王三达, 段晓侠, 蔡晓兵, 等, 2023. 大别造山带石关地区变质岩风化壳中REY富集和分异研究[J]. 地质与勘探, 59(4): 828-851. doi: 10.12134/j.dzykt.2023.04.011
    [84]
    王雅萍, 鲍志东, 张连进, 等, 2024. 四川盆地蓬莱地区埃迪卡拉系灯影组二段微生物岩储层成岩作用: 对优质储层形成与演化的启示[J]. 地质力学学报, 30(4): 579-594
    [85]
    吴元保, 郑永飞, 2004. 锆石成因矿物学研究及其对U-Pb年龄解释的制约[J]. 科学通报, 49(16): 1589-1604. doi: 10.3321/j.issn:0023-074X.2004.16.002
    [86]
    熊家镛, 张志斌, 刘世荣, 等, 1980. 中华人民共和国1: 20万区域地质调查报告(东川幅)[R]. 玉溪: 云南省地质局.
    [87]
    徐云飞, 2018. 滇中易门地区古元古界的厘定及区域找矿意义[D]. 昆明: 昆明理工大学.
    [88]
    杨永祯, 郭岭, 方泽鑫, 等, 2024. 康滇古陆东缘筇竹寺组沉积物源的风化特征: 以云南省楚雄市武定县乌龙村剖面为例[J]. 沉积学报, 42(1): 324-341. doi: 10.14027/j.issn.1000-0550.2022.073
    [89]
    云南省地质矿产局, 1990. 云南省区域地质志[M]. 北京: 地质出版社.
    [90]
    占沈薇, 2023. 扬子板块西缘泸沽花岗岩的地球化学特征及地质意义[D]. 成都: 成都理工大学.
    [91]
    张冬孟, 程鑫, 卫弼天, 等, 2023. 滇东地区寒武系第三阶沉积岩磁组构研究及其对古水流方向的启示[J]. 西北大学学报(自然科学版), 53(4): 655-670. doi: 10.16152/j.cnki.xdxbzr.2023-04-016
    [92]
    张克信, 潘桂棠, 何卫红, 等, 2015. 中国构造-地层大区划分新方案[J]. 地球科学—中国地质大学学报, 40(2): 206-233.
    [93]
    张克信, 何卫红, 徐亚东, 等, 2023. 华南青白口纪–三叠纪构造–地层区划及特征[J]. 华南地质, 39(1): 1-23.
    [94]
    张帅, 罗冰, 汪泽成, 等, 2025. 四川盆地德阳-安岳克拉通内裂陷成因及其与原特提斯洋的联系[J]. 天然气工业, 45(2): 37-50. doi: 10.3787/j.issn.1000-0976.2025.02.004
    [95]
    张英利, 贾晓彤, 王宗起, 等, 2018. 米仓山地区早寒武世仙女洞组沉积物源新认识: 沉积学、重矿物和碎屑锆石年代学的证据[J]. 地质学报, 92(9): 1918-1935. doi: 10.3969/j.issn.0001-5717.2018.09.011
    [96]
    赵国春, 韩以贵, 李建华, 等, 2022. 超大陆聚散的环境效应[J]. 地质学报, 96(9): 3120-3127. doi: 10.3969/j.issn.0001-5717.2022.09.010
    [97]
    周明忠, 罗泰义, 黄智龙, 等, 2011. 贵州早寒武世火山活动记录及其地质意义[J]. 矿物学报, 31(3): 453-461.
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