Qingdao Institute of marine geology, China Geological SurveyHost
Advanced Search
Previous Article Next Article
2024 Vol. 40, No. 12
Article Contents
Article navigation > Marine Geology Frontiers > 2024 > 40(12): 50-63
Next Article Previous Article

HE Anbei, ZHU Zuofei, ZHAO Qi. Cretaceous paleoclimate evolution of Yong'an Basin in western Fujian and its response to geomorphic changes along the coast of South China[J]. Marine Geology Frontiers, 2024, 40(12): 50-63. doi: 10.16028/j.1009-2722.2023.220
Citation: HE Anbei, ZHU Zuofei, ZHAO Qi. Cretaceous paleoclimate evolution of Yong'an Basin in western Fujian and its response to geomorphic changes along the coast of South China[J]. Marine Geology Frontiers, 2024, 40(12): 50-63. doi: 10.16028/j.1009-2722.2023.220
shu

Cretaceous paleoclimate evolution of Yong'an Basin in western Fujian and its response to geomorphic changes along the coast of South China

  • 1.

    Key Laboratory of Ocean and Marginal Sea Geology, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China

  • 2.

    Center for Excellence in Deep Earth Science, Chinese Academy of Sciences, Guangzhou 510640, China

  • 3.

    College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing 100049, China

  • 4.

    Faculty of Geography, Yunnan Normal University, Kunming 650500, China

  • 5.

    Sanya Institute of South China Sea Geology, Guangzhou Marine Geological Survey, Sanya 572025, China

Received Date:  20 March 2022
Publish Date:  28 December 2024
    Abstract

  • To explore the evolution characteristics of the Cretaceous paleoclimate in the Yong'an Basin in western Fujian and the influence of the Late Mesozoic geomorphic changes along the coast of South China on the paleoclimate in the southeastern margin of South China, the Cretaceous stratigraphy of the Bantou, Shaxian, and Chong'an formations in the basin was taken as the research object. The fine-grained clastic rock samples were collected and examined for major and trace elements and rare earth elements distributions, and their sedimentary and paleontological characteristics were compared and analyzed. Variations in the paleoclimate of the Yong'an Basin in western Fujian during the Cretaceous period were clarified. Results show that the early Cretaceous Bantou Formation reflects a changing climate condition. The value ranges of CIA (chemical index of alteration) (69.91～85.29), Rb/Sr (1.13～2.21), Mg/Ca (0.57～3.57), Sr/Cu (5.44～11.66), and the calibrated paleosalinity index [100*Sr/(BaAl2O3)] (CPI) (1.18～1.55) collectively suggest a scheme transition from a warm-humid climate to a dry-hot environment. Moreover, the redox discrimination indices δCe (0.89～1.03), V/Cr (1.03～1.57), and Ni/Co (2.34～10.58) signaled a dominant weak oxidation environment, aligning with the transition to dry-hot climate in the early Cretaceous. Moving to the late Early Cretaceous to Late Cretaceous, Shaxian Formation and Chong'an Formation samples manifest further shifts in climate dynamics. The value ranges of CIA (67.14～75.68), Rb/Sr (0.99～9.05), Mg/Ca (0.37～16.22), Sr/Cu (1.20～15.46), and CPI (0.50-1.77) expose a change from hot-dry to warm-humid, followed by a transition to cold-dry climate. The δCe value (0.89～1.03), V/Cr (0.51～1.72), and Ni/Co (1.45～6.45) point to alternating weak oxidation and weak reduction environments, aligning with the multiple climate shifts during this period. Therefore, the Cretaceous paleoclimate of the Yong'an Basin exhibits a complex transitional sequence in climate, oscillating from dry-hot to warm-humid and then to dry-cold conditions, often with extreme climates. By comparing the paleoclimate between the study area and the surrounding South China region, it is evident that the predominant transformation in the inland South China paleoclimate was from warm-wet to dry-hot conditions. The paleoclimate transitions between the coastal and inland regions of South China reflect the response to late Mesozoic coastal geomorphic changes in the South China coastal areas.

    • FullText(HTML)
  • 加载中
    • References
  • [1] CHEN Y,MENG J,LIU H,et al. Detrital zircons record the evolution of the Cathaysian Coastal Mountains along the South China margin[J]. Basin Research,2022,34(2):688-701.

    Google Scholar

    [2] 陈丕基. 晚白垩世中国东南沿岸山系与中南地区的沙漠和盐湖化[J]. 地层学杂志,1997,21(3):44-54.

    Google Scholar

    CHEN P J. Coastal Mountains of SE China,desertization and saliniferous lakes of Central China during the Upper Cretaceous[J]. Journal of Stratigraphy,1997,21(3):44-54.

    Google Scholar

    [3] CHEN P J. Paleoenvironmental changes during the Cretaceous in eastern China [M]//OKADA H,MATEER N J. Cretaceous Environments of Asia. Elsevier,2000:81-90.

    Google Scholar

    [4] LI J H,ZHANG Y Q,DONG S W,et al. Cretaceous tectonic evolution of South China:a preliminary synthesis[J]. Earth-Science Reviews,2014,134:98-136. doi: 10.1016/j.earscirev.2014.03.008

    CrossRef Google Scholar

    [5] YAN Y,HU X Q,LIN G,et al. Sedimentary provenance of the Hengyang and Mayang basins,SE China,and implications for the Mesozoic topographic change in South China Craton:evidence from detrital zircon geochronology[J]. Journal of Asian Earth Sciences,2011,41(6):494-503. doi: 10.1016/j.jseaes.2011.03.012

    CrossRef Google Scholar

    [6] TAN J,ZHANG L,WANG C,et al. Late Cretaceous provenance change in the Jiaolai Basin,East China:implications for paleogeographic evolution of East Asia[J]. Journal of Asian Earth Sciences,2020,194:104188. doi: 10.1016/j.jseaes.2019.104188

    CrossRef Google Scholar

    [7] 陈云华. 中国东南地区晚白垩世沉积响应与古气候 [D]. 成都:成都理工大学,2008.

    Google Scholar

    CHEN Y H. Late Cretaceous sedimentary responses to the “Coast Range" and paleoclimatechanges in Southeast China [D]. Chengdu:Chengdu University of Technolog,2008.

    Google Scholar

    [8] LI X M,ZOU H P. Late Cretaceous-Cenozoic exhumation of the southeastern margin of Coastal Mountains,SE China,revealed by fission-track thermochronology:implications for the topographic evolution[J]. Solid Earth Sciences,2017,2(3):79-88. doi: 10.1016/j.sesci.2017.02.001

    CrossRef Google Scholar

    [9] DING R X,MIN K,ZOU H P. Inversion of topographic evolution using low-T thermal history:a case study from coastal mountain system in southeastern China[J]. Gondwana Research,2019,67:21-32. doi: 10.1016/j.gr.2018.09.009

    CrossRef Google Scholar

    [10] WANG Y,WANG Y J,LI S B,et al. Exhumation and landscape evolution in eastern South China since the Cretaceous:new insights from fission-track thermochronology[J]. Journal of Asian Earth Sciences,2020,191:104239. doi: 10.1016/j.jseaes.2020.104239

    CrossRef Google Scholar

    [11] 冯连君,储雪蕾,张同钢,等. 莲沱砂岩:南华大冰期前气候转冷的沉积记录[J]. 岩石学报,2006,22(9):2387-2393.

    Google Scholar

    FENG L J,CHU X L,ZHANG T G,et al. Liantuo sandstones:sedimentary records under cold climate before the Nanhua big glaciations[J]. Acta Petrologica Sinica,2006,22(9):2387-2393.

    Google Scholar

    [12] 王随继,黄杏珍,妥进才,等. 泌阳凹陷核桃园组微量元素演化特征及其古气候意义[J]. 沉积学报,1997,15(1):66-71.

    Google Scholar

    WANG S J,HUANG X Z,TUO J C,et al. Evolutional characteristics and their paleoclimate significance of trace elements in the Hetaoyuan Formation,Biyang Depression[J]. Acta Sedimentologica Sinica,1997,15(1):66-71.

    Google Scholar

    [13] 许中杰,程日辉,沈艳杰,等. 闽西南地区晚三叠—早侏罗世温湿-干热气候转变的沉积记录 [J]. 中国矿业大学学报,2012,41(5):783-792.

    Google Scholar

    XU Z J,CHENG R H,SHEN Y J,et al. Sedimentary records of the climatic transition from warm and humid to dry and hot during Late Triassic-Early Jurassic in southwestern Fujian [J]. Journal of China University of Mining & Technology,2012,41(5):783-792.

    Google Scholar

    [14] 徐崇凯,刘池洋,郭佩,等. 潜江凹陷古近系潜江组盐间泥岩地球化学特征及地质意义[J]. 沉积学报,2018,36(3):617-629.

    Google Scholar

    XU C K,LIU C Y,GUO P,et al. Geochemical characteristics and their geological significance of intrasalt mudstones from the Paleogene Qianjiang Formation in the Qianjiang Graben,Jianghan Basin,China[J]. Acta Sedimentologica Sinica,2018,36(3):617-629.

    Google Scholar

    [15] 陈佩蓉,许中杰,孔锦涛,等. 闽西南地区中侏罗世古气候演化及其对华南构造体制转换的响应[J]. 大地构造与成矿学,2020,44(5):1012-1024.

    Google Scholar

    CHEN P R,XU Z J,KONG J T,et al. Paleoclimatic evolution during Middle Jurassic in southwestern Fujian and its responses to the tectonic regime transition in South China[J]. Geotectonica et Metallogenia,2020,44(5):1012-1024.

    Google Scholar

    [16] 陈森然,许中杰,孔锦涛,等. 华南陆缘粤南地区晚三叠世—早、中侏罗世古气候演化及其对华南构造体制转换的响应[J]. 地球科学,2021,46(9):3290-3306.

    Google Scholar

    CHEN S R,XU Z J,KONG J T,et al. Paleoclimatic evolution during Late Triassic-Early-Middle Jurassic in South Guangdong of South China continental margin and its responses to the tectonic regime transition[J]. Earth Science,2021,46(9):3290-3306.

    Google Scholar

    [17] 李祥辉,陈斯盾,曹珂,等. 浙闽地区白垩纪中期古土壤类型与古气候 [J]. 地学前缘,2009,16(5):63-70.

    Google Scholar

    LI X H,CHEN S D,CAO K,et al. Paleosols of the mid-Cretaceous:a report from Zhejiang and Fujian ,SE China [J]. Earth Science Frontiers ,2009 ,16(5):63-70.

    Google Scholar

    [18] 刘玲,李祥辉,王尹,等. 浙闽地区白垩纪早中期黏土矿物组成特征及其古气候显示[J]. 沉积学报,2012,30(1):120-127.

    Google Scholar

    LIU L,LI X H,WANG Y,et al. The Early-Mid Cretaceous changes of clay mineral composition from Zhejiang and Fujian Provinces,SE China:indications to paleoclimate changes[J]. Acta Sedimentologica Sinica,2012,30(1):120-127.

    Google Scholar

    [19] 刘友祥,胡文瑄,胡广. 浙闽地区早白垩世暗色岩系的孢粉组合与古气候特征[J]. 高校地质学报,2014,20(4):590-601.

    Google Scholar

    LIU Y X,HU W X,HU G. Spores and pollen assemblages and their paleo-climate implication from the Early Cretaceous dark mudstone in Zhejiang and Fujian Provinces[J]. Geological Journal of China Universities,2014,20(4):590-601.

    Google Scholar

    [20] CHARVET J,SHU L S,SHI Y S,et al. The building of South China:collision of Yangzi and Cathaysia blocks,problems and tentative answers[J]. Journal of Southeast Asian Earth Sciences,1996,13(3/5):223-235.

    Google Scholar

    [21] SHU L,CHARVET J. Kinematics and geochronology of the proterozoic Dongxiang-Shexian ductile shear zone:with HP metamorphism and ophiolitic melange (Jiangnan region,South China)[J]. Tectonophysics,1996,267(1/4):291-302.

    Google Scholar

    [22] WANG X L,ZHOU J C,GRIFFIN W L,et al. Detrital zircon geochronology of Precambrian basement sequences in the Jiangnan orogen:dating the assembly of the Yangtze and Cathaysia Blocks[J]. Precambrian Research,2007,159(1/2):117-131.

    Google Scholar

    [23] WANG Y,FAN W,CAWOOD P A,et al. Indosinian high-strain deformation for the Yunkaidashan tectonic belt,South China:kinematics and 40Ar/ 39Ar geochronological constraints [J]. Tectonics,2007,26(6):TC6008.

    Google Scholar

    [24] ZHOU J C,WANG X L,QIU J S. Geochronology of Neoproterozoic mafic rocks and sandstones from northeastern Guizhou,South China:coeval arc magmatism and sedimentation[J]. Precambrian Research,2009,170(1):27-42.

    Google Scholar

    [25] ZHONG D L. Paleotethysides in West Yunnan and Sichuan,China [M]. Beijing: China Science Press,2000.

    Google Scholar

    [26] WANG Y J,FAN W M,ZHANG G W,et al. Phanerozoic tectonics of the South China Block:key observations and controversies[J]. Gondwana Research,2013,23(4):1273-1305. doi: 10.1016/j.gr.2012.02.019

    CrossRef Google Scholar

    [27] LI J H,MA Z L,ZHANG Y Q,et al. Tectonic evolution of Cretaceous extensional basins in Zhejiang Province,eastern South China:structural and geochronological constraints[J]. International Geology Review,2014,56(13):1602-1629. doi: 10.1080/00206814.2014.951978

    CrossRef Google Scholar

    [28] LI X H. Cretaceous magmatism and lithospheric extension in Southeast China[J]. Journal of Asian Earth Sciences,2000,18(3):293-305. doi: 10.1016/S1367-9120(99)00060-7

    CrossRef Google Scholar

    [29] ZHOU X M,LI W X. Origin of Late Mesozoic igneous rocks in Southeastern China:implications for lithosphere subduction and underplating of mafic magmas[J]. Tectonophysics,2000,326(3):269-287.

    Google Scholar

    [30] 毛景文, 谢桂青, 李晓峰, 等. 华南地区中生代大规模成矿作用与岩石圈多阶段伸展[J]. 地学前缘, 2004, 11(1): 45-55.

    Google Scholar

    MAO J W, XIE G Q, LI X F, et al. Mesozoic large scale mineralization and multiple lithospheric extension in South China.[J]. Earth Science Frontiers, 2004, 11(1): 45-55.

    Google Scholar

    [31] MAO J W,WANG Y T,LEHMANN B,et al. Molybdenite Re-Os and albite 40Ar/39Ar dating of Cu-Au-Mo and magnetite porphyry systems in the Yangtze River valley and metallogenic implications[J]. Ore Geology Reviews,2006,29(3):307-324.

    Google Scholar

    [32] ZHOU X M,SUN T,SHEN W Z,et al. Petrogenesis of Mesozoic granitoids and volcanic rocks in South China:a response to tectonic evolution[J]. International Union of Geological Sciences,2006,29(1):26-33.

    Google Scholar

    [33] LI Z X,LI X H. Formation of the 1300-km-wide intracontinental orogen and postorogenic magmatic province in Mesozoic South China:a flat-slab subduction model[J]. Geology,2007,35(2):179-182. doi: 10.1130/G23193A.1

    CrossRef Google Scholar

    [34] HU R Z,BI X W,ZHOU M F,et al. Uranium metallogenesis in South China and its relationship to crustal extension during the Cretaceous to Tertiary[J]. Economic Geology,2008,103(3):583-598. doi: 10.2113/gsecongeo.103.3.583

    CrossRef Google Scholar

    [35] SHU L S,ZHOU X M,DENG P,et al. Mesozoic tectonic evolution of the Southeast China Block:new insights from basin analysis[J]. Journal of Asian Earth Sciences,2009,34(3):376-391. doi: 10.1016/j.jseaes.2008.06.004

    CrossRef Google Scholar

    [36] CHU Y,LIN W,FAURE M,et al. Cretaceous episodic extension in the South China Block,East Asia:evidence from the Yuechengling Massif of Central South China[J]. Tectonics,2019,38(10):3675-3702. doi: 10.1029/2019TC005516

    CrossRef Google Scholar

    [37] LI J,CAWOOD P A,RATSCHBACHER L,et al. Building Southeast China in the Late Mesozoic:insights from alternating episodes of shortening and extension along the Lianhuashan Fault Zone[J]. Earth-Science Reviews,2020,201:103056. doi: 10.1016/j.earscirev.2019.103056

    CrossRef Google Scholar

    [38] YAN D P,ZHOU M F,SONG H L,et al. Origin and tectonic significance of a Mesozoic multi-layer over-thrust system within the Yangtze Block (South China)[J]. Tectonophysics,2003,361(3):239-254.

    Google Scholar

    [39] LIN W,WANG Q C,CHEN K. Phanerozoic tectonics of South China Block:new insights from the polyphase deformation in the Yunkai massif [J]. Tectonics,2008,27(6):TC6004

    Google Scholar

    [40] LI J H,DONG S W,CAWOOD P A,et al. An Andean-type retro-arc foreland system beneath northwest South China revealed by SINOPROBE profiling[J]. Earth and Planetary Science Letters,2018,490:170-179. doi: 10.1016/j.jpgl.2018.03.008

    CrossRef Google Scholar

    [41] SUN W D,LING M X,YANG X Y,et al. Ridge subduction and porphyry copper-gold mineralization:an overview[J]. Science China (Earth Sciences),2010,53(4):475-484. doi: 10.1007/s11430-010-0024-0

    CrossRef Google Scholar

    [42] WANG Z H,LU H F. Ductile deformation and 40Ar/39Ar dating of the Changle–Nanao ductile shear zone,southeastern China[J]. Journal of Structural Geology,2000,22(5):561-570. doi: 10.1016/S0191-8141(99)00179-0

    CrossRef Google Scholar

    [43] WEI W,FAURE M,CHEN Y,et al. Back-thrusting response of continental collision:Early Cretaceous NW-directed thrusting in the Changle-Nan'ao Belt (Southeast China)[J]. Journal of Asian Earth Sciences,2015,100:98-114. doi: 10.1016/j.jseaes.2015.01.005

    CrossRef Google Scholar

    [44] 祖辅平,舒良树,李成. 永安盆地晚古生代—中—新生代沉积构造环境演化特征[J]. 地质论评,2012,58(1):126-148.

    Google Scholar

    ZU F P,SHU L S,LI C. Evolution features of depositional and tectonic setting from Late Paleozoic to Meso-Cenozoic in the Yong’an Basin[J]. Geological Review,2012,58(1):126-148.

    Google Scholar

    [45] HU L S,CAWOOD P A,DU Y S,et al. Late Paleozoic to Early Mesozoic provenance record of paleo-Pacific subduction beneath South China[J]. Tectonics,2015,34(5):986-1008. doi: 10.1002/2014TC003803

    CrossRef Google Scholar

    [46] 陈金秀. 福建省永安盆地第四纪冰川遗迹的探讨 [J]. 福建地质,1984 (1):61-67.

    Google Scholar

    CHEN J X. Exploration of Quaternary glacier relics in Yong'an Basin,Fujian Province [J]. Geology of Fujian,1984(1):61-67.

    Google Scholar

    [47] 李兼海. 福建省岩石地层 [M]. 北京:中国地质大学出版社,1997.

    Google Scholar

    LI J H. Geological Strata of Fujian Province [M]. Beijing:China University of Geosciences Press,1997.

    Google Scholar

    [48] XU Q J,LIU S F,WANG Z F,et al. Provenance of the East Guangdong Basin and Yong'an Basin in Southeast China:response to the Mesozoic tectonic regime transformation[J]. Journal of Asian Earth Sciences,2019,185:104024. doi: 10.1016/j.jseaes.2019.104024

    CrossRef Google Scholar

    [49] LI X H,ZHANG C K,LI Y X,et al. Refined chronostratigraphy of the Late Mesozoic terrestrial strata in South China and its tectono-stratigraphic evolution[J]. Gondwana Research,2019,66:143-167. doi: 10.1016/j.gr.2018.09.006

    CrossRef Google Scholar

    [50] FREYDIER R,MICHARD A,DE LANGE G,et al. Nd isotopic compositions of eastern Mediterranean sediments:tracers of the Nile influence during sapropel S1 formation?[J]. Marine Geology,2001,177(1):45-62.

    Google Scholar

    [51] 赵振华. 微量元素地球化学原理 [M]. 北京:科学出版社,2016.

    Google Scholar

    ZHAO Z H. Geochemistry of trace elements [M] . Beijing:Science Press,2016.

    Google Scholar

    [52] NESBITT H W,YOUNG G M. Early Proterozoic climates and plate motions inferred from major element chemistry of lutites[J]. Nature,1982,299(5885):715-717. doi: 10.1038/299715a0

    CrossRef Google Scholar

    [53] 何岸北. 东南沿海古海岸山脉演化:永安盆地晚中生代沉积及古气候响应 [D]. 广州:中国科学院大学(中国科学院广州地球化学研究所),2022.

    Google Scholar

    HE A B. Evolution of Paleo-Coastal Mountains along the Southeast Coast:Sedimentation and Paleoclimate Response in Yong'an Basin of the Late Mesozoic [D]. Guangzhou:University of Chinese Academy of Sciences (Guangzhou Institute of Geochemistry,Chinese Academy of Sciences),2022.

    Google Scholar

    [54] MCLENNAN S M,HEMMING S,MCDANIEL D K,et al. Geochemical Approaches to Sedimentation,Provenance,and Tectonics [M]//JOHNSSON M J,BASU A. Processes Controlling the Composition of Clastic Sediments. Geological Society of America,1993:21-40.

    Google Scholar

    [55] CHEN J,AN Z S,HEAD J. Variation of Rb/Sr ratios in the loess-paleosol sequences of Central China during the last 130,000 years and their implications for monsoon paleoclimatology[J]. Quaternary Research,1999,51(3):215-219. doi: 10.1006/qres.1999.2038

    CrossRef Google Scholar

    [56] CHEN J,WANG Y J,CHEN Y,et al. Rb and Sr geochemical characterization of the Chinese loess stratigraphy and its implications for palaeomonsoon climate[J]. Acta Geologica Sinica (English Edition),2000,74(2):279-288. doi: 10.1111/j.1755-6724.2000.tb00462.x

    CrossRef Google Scholar

    [57] 田景春,张翔. 沉积地球化学 [M]. 北京:地质出版社,2016.

    Google Scholar

    TIAN J C,ZHANG X. Sedimentary geochemistry [M]. Beijing:Geology Press,2016.

    Google Scholar

    [58] 田晓雪,雒昆利,谭见安,等. 黑龙江嘉荫地区白垩系与古近系界线附近的古气候分析 [J]. 古地理学报,2005,7(3):425-432.

    Google Scholar

    TIAN X X,LUO K L,TAN J A,et al. Analysis on palaeoclimate neighbouring the Cretaceous and Paleogene boundary in Jiayin area,Heilongjiang Province [J]. Journal of Palaeogeography,2005,7(3):425-432.

    Google Scholar

    [59] 王益友,郭文莹,张国栋. 几种地球化学标志在金湖凹陷阜宁群沉积环境中的应用[J]. 同济大学学报,1979(2):51-60.

    Google Scholar

    WANG Y Y,GUO W Y,ZHANG G D. Application of some geochemical indicators in determiring of sedimentary environment of the Funing Group (Paleogene),Jinhu Depression,Kiangsu Province[J]. Journal of Tongji University,1979(2):51-60.

    Google Scholar

    [60] 王敏芳,焦养泉,王正海,等. 沉积环境中古盐度的恢复:以吐哈盆地西南缘水西沟群泥岩为例[J]. 新疆石油地质,2005,26(6):117-120.

    Google Scholar

    WANG M F,JIAO Y Q,WANG Z H. Recovery paleosalinity in sedimentary environment: an example of mudstone in Shuixigou Group,southwestern margin of Turpan-Hami Basin[J]. Xinjiang Petroleum Geology,2005,26(6):117-120.

    Google Scholar

    [61] WRIGHT J,SCHRADER H,HOLSER W T. Paleoredox variations in ancient oceans recorded by rare earth elements in fossil apatite[J]. Geochimica et Cosmochimica Acta,1987,51(3):631-644. doi: 10.1016/0016-7037(87)90075-5

    CrossRef Google Scholar

    [62] JONES B,MANNING D A C. Comparison of geochemical indices used for the interpretation of palaeoredox conditions in ancient mudstones[J]. Chemical Geology,1994,111(1):111-129.

    Google Scholar

    [63] WIGNALL P B,TWITCHETT R J. Oceanic anoxia and the end Permian mass extinction[J]. Science,1996,272(5265):1155-1158. doi: 10.1126/science.272.5265.1155

    CrossRef Google Scholar

    [64] 吴朝东,杨承运,陈其英. 湘西黑色岩系地球化学特征和成因意义 [J]. 岩石矿物学杂志,1999,18(1):28-29,31-41.

    Google Scholar

    WU C D,YANG C Y,CHEN Q Y. The origin and geochemical characteristics of Upper Sinain Lower Cambrian black shales in western Hunan [J]. Acta Petrologica et Mineralogica1999,18 (1):28-29,31-41.

    Google Scholar

    [65] RIMMER S M. Geochemical paleoredox indicators in Devonian-Mississippian black shales,Central Appalachian Basin (USA)[J]. Chemical Geology,2004,206(3):373-391.

    Google Scholar

    [66] SCHEFFLER K,BUEHMANN D,SCHWARK L. Analysis of late Palaeozoic glacial to postglacial sedimentary successions in South Africa by geochemical proxies:response to climate evolution and sedimentary environment[J]. Palaeogeography,Palaeoclimatology,Palaeoecology,2006,240(1):184-203.

    Google Scholar

    [67] 彭华,吴志才. 关于红层特点及分布规律的初步探讨 [J]. 中山大学学报(自然科学版),2003,42(5):109-113.

    Google Scholar

    PENG H ,WU Z C. A preliminary study on the characteristics and the distribution of red beds [J]. Acta Scientiarum Naturalium Universitatis SunYatseni,2003,42(5):109-113.

    Google Scholar

    [68] DOUGLAS P M J,BRENNER M,Curtis J H. Methods and future directions for paleoclimatology in the Maya lowlands[J]. Global and Planetary Change,2016,138:3-24. doi: 10.1016/j.gloplacha.2015.07.008

    CrossRef Google Scholar

    [69] 刘秀铭,吕镔,毛学刚,等. 风积地层中铁矿物随环境变化及其启示[J]. 第四纪研究,2014,34(3):443-457.

    Google Scholar

    LIU X M,LYV B,MAO X G,et al. Iron minerals of aeolian deposits vary with environment and its significances[J]. Quaternary Sciences,2014,34(3):443-457.

    Google Scholar

    [70] TEWARI R,CHATTERJEE S,AGNIHOTRI D,et al. Glossopteris flora in the Permian Weller Formation of Allan Hills,South Victoria Land,Antarctica:implications for paleogeography,paleoclimatology,and biostratigraphic correlation[J]. Gondwana Research,2015,28(3):905-932. doi: 10.1016/j.gr.2015.02.003

    CrossRef Google Scholar

    [71] 邓胜徽,卢远征,赵怡,等. 中国侏罗纪古气候分区与演变[J]. 地学前缘,2017,24(1):106-142.

    Google Scholar

    DENG S H,LU Y Z,ZHAO Y,et al. The Jurassic palaeoclimate regionalization and evolution of China[J]. Earth Science Frontiers,2017,24(1):106-142.

    Google Scholar

    [72] 岳来群,游国庆,郑宁,等. 福建坂头组沉积特征及构造背景研究[J]. 中国地质,2011,38(5):1220-1231.

    Google Scholar

    YUE L Q,YOU G Q,ZHENG N,et al. Sedimentary characteristics and tectonic background of Bantou period in Fujian[J]. Geology in China,2011,38(5):1220-1231.

    Google Scholar

    [73] 梁诗经,文斐成,陈润生,等. 福建泰宁白垩纪红层植物及孢粉化石组合特征[J]. 福建地质,2006(1):1-9.

    Google Scholar

    LIANG S J,WEN F C,CHEN R S. The assemblage and characters of floras and sporo-pollen fossils in the Cretaceous red-bed basin of Taining County,Fujian Province[J]. Geology of Fujian,2006(1):1-9.

    Google Scholar

    [74] 福建省地质调查研究院. 中国区域地质志:福建志 [M]. 北京:地质出版社,2016.

    Google Scholar

    Fujian Institute Of Geological Survey. Regional Geology of China:Fujian Province [M]. Beijing:Geology Press,2016.

    Google Scholar

    [75] HU G,HU W X,CAO J,et al. Deciphering the Early Cretaceous transgression in coastal southeastern China:constraints based on petrography,paleontology and geochemistry[J]. Palaeogeography,Palaeoclimatology,Palaeoecology,2012,317/318:182-195.

    Google Scholar

    [76] 刘静,张金玉,葛玉魁,等. 构造地貌学:构造-气候-地表过程相互作用的交叉研究 [J]. 科学通报,2018,63(30):3070-3088.

    Google Scholar

    LIU J,ZHANG J Y,GE Y K,et al. Tectonic geomorphology:an interdisciplinary study of the interaction among tectonic climatic and surface processes[J]. Chinese Science Bulletin,2018,63(30):3070-3088.

    Google Scholar

    [77] 刘芮岑. 湖南茶陵盆地晚白垩世—古新世古气候分析 [D]; 南京大学,2018.

    Google Scholar

    LIU R C. Paleoclimate of the Late Cretaceous-Paleocene in the Chaling Basin,Hunan,South China [D]. Nanjing:Nanjing University,2018.

    Google Scholar

    [78] 黄乐清,黄建中,罗来,等. 湖南衡阳盆地东缘白垩系风成沉积的发现及其古环境意义[J]. 沉积学报,2019,37(4):735-748.

    Google Scholar

    HUANG Y Q,HUANG J Z,LUO L,et al. The discovery of Cretaceous eolian deposits at the eastern margin of the Hengyang Basin,Hunan,and its paleoenvironmental significance[J]. Acta Sedimentologica Sinica,2019,37(4):735-748.

    Google Scholar

    [79] TENG X H,FANG X M,KAUFMAN A J,et al. Sedimentological and mineralogical records from drill core SKD1 in the Jianghan Basin,Central China,and their implications for late Cretaceous-Early Eocene climate change[J]. Journal of Asian Earth Sciences,2019,182:103936.1-103936.14.

    Google Scholar

    [80] CHEN L Q,STEEL R J,GUO F S,et al. Alluvial fan facies of the Yongchong Basin:implications for tectonic and paleoclimatic changes during Late Cretaceous in SE China[J]. Journal of Asian Earth Sciences,2017,134:37-54. doi: 10.1016/j.jseaes.2016.10.010

    CrossRef Google Scholar

    [81] 李余亮. 广东省韶关市丹霞盆地长坝组沉积特征与古气候研究 [D]. 抚州:东华理工大学,2018.

    Google Scholar

    LI Y L. Sedimentary Characteristics and Paleoclimate of the Changba Formation in the Danxia Basin,Shaoguan City,Guangdong Province,South China [D]. Fuzhou:East China University of Technology,2018.

    Google Scholar

    [82] 王文艳,刘秀铭,马明明,等. 南雄盆地白垩纪红层沉积环境分析[J]. 亚热带资源与环境学报,2016,11(3):29-37.

    Google Scholar

    WANG W Y,LIU X M,MA M M,et a1. Sedimentary environment of Cretaceous red beds in Nanxiong Basin,Guangdong Province[J]. Journal of Subtropical Resources and Environment,2016,11(3):29-37.

    Google Scholar

    [83] 张哲. 三水盆地下白垩统—始新统黏土矿物特征及其对区域构造-气候事件的响应 [D]. 北京:中国地质大学(北京),2018.

    Google Scholar

    ZHANG Z. Clay Mineral Characteristics of Sanshui BasinfromLower Cretaceous to Eocene and Their Response to Tectonic Activities and Climate Changes in the Region [D]. Beijing:China University of Geosciences (Beijing ),2018.

    Google Scholar

    [84] 梁西文. 中扬子区晚三叠世—新近纪层序岩相古地理演化研究 [D]. 成都:成都理工大学,2008.

    Google Scholar

    LIANG X W. Study on Lithofacies Paleographic Evolution of Late Triassic-Neogene Sequence in Mid-Yangtze Region [D]. Chengdu:Chengdu University of Technology,2008.

    Google Scholar

    [85] 王宇佳. 江西广丰晚白垩世周田组沉积特征与古气候分析 [D]. 抚州:东华理工大学,2019.

    Google Scholar

    WANG Y J. Sedimentary Characteristics and Paleoclimate of the Zhoutian Formation in the Guangfeng Basin of Jiangxi Province [D]. Fuzhou:East China University of Technology,2019

    Google Scholar

    [86] 刘友祥. 浙闽地区下白垩统暗色岩系的沉积环境研究 [D]. 南京:南京大学,2012.

    Google Scholar

    LIU Y X. Study of Sedimentary Environment of Dark Sedimentary Rocks in Lower Cretaceous,Zhejiang and Fujian Provinces [D]. Nanjing:Nanjing University,2012.

    Google Scholar

    • Relative Articles
  • Cited by
  • Supplements
    • Proportional views
  • 加载中
通讯作者: 陈斌, bchen63@163.com
  • 1. 

    沈阳化工大学材料科学与工程学院 沈阳 110142

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索

Figures(4)

Tables(2)

Export Citation
PDF
XML

Article Metrics

Article views(89) PDF downloads(2) Cited by(0)

Access History

Other Articles By Authors

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    版权所有：中国地质调查局发展研究中心 copyright @2020