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南雄盆地晚白垩世—古新世陆源沉积组份变化的古气候指示

王尹 李祥辉 周勇 刘玲

王尹, 李祥辉, 周勇, 刘玲. 南雄盆地晚白垩世—古新世陆源沉积组份变化的古气候指示[J]. 沉积学报, 2015, 33(1): 116-123. doi: 10.14027/j.cnki.cjxb.2015.01.012
引用本文: 王尹, 李祥辉, 周勇, 刘玲. 南雄盆地晚白垩世—古新世陆源沉积组份变化的古气候指示[J]. 沉积学报, 2015, 33(1): 116-123. doi: 10.14027/j.cnki.cjxb.2015.01.012
WANG Yin, LI XiangHui, ZHOU Yong, LIU Ling. Paleoclimate Indication of Terrigenous Clastic Rock's Component during the Late Cretaceous-Early Paleocene in the Nanxiong Basin[J]. Acta Sedimentologica Sinica, 2015, 33(1): 116-123. doi: 10.14027/j.cnki.cjxb.2015.01.012
Citation: WANG Yin, LI XiangHui, ZHOU Yong, LIU Ling. Paleoclimate Indication of Terrigenous Clastic Rock's Component during the Late Cretaceous-Early Paleocene in the Nanxiong Basin[J]. Acta Sedimentologica Sinica, 2015, 33(1): 116-123. doi: 10.14027/j.cnki.cjxb.2015.01.012

南雄盆地晚白垩世—古新世陆源沉积组份变化的古气候指示

doi: 10.14027/j.cnki.cjxb.2015.01.012
基金项目: 国家自然科学基金项目(批准号:41372106)和国际重点基础研究发展计划“973”项目(编号:2012CB822003)联合资助
详细信息
    作者简介:

    王尹 男 1985年出生 硕士 古气候与古土壤 E-mail: yin31721@qq.com

  • 中图分类号: P532

Paleoclimate Indication of Terrigenous Clastic Rock's Component during the Late Cretaceous-Early Paleocene in the Nanxiong Basin

  • 摘要: 利用陆源沉积中的碎屑组份(泥岩中的碎屑黏土矿物种类和砂岩中砂、粉砂碎屑类型)相对含量变化,对广东北部和江西南部的南雄盆地晚白垩世—古新世古气候进行了分析.结果显示,砂岩碎屑组份含量气候指数(长石/石英比,F/Q)介于0.02~0.14之间;(碎屑)黏土矿物组合主要以伊利石为主,平均79%;伊利石结晶度指数与化学指数分别为0.25~0.39、0.31~0.7.进一步分析表明,研究区这一时期以干旱气候为主,存在暖湿气候间断,古气候演化可分为三个阶段:晚白垩世马斯特里赫特期以干旱—半干旱性气候为主,古新世丹尼期早期转变为相对湿热或与干旱—半干旱气候交替,古新世丹尼期晚期恢复到半干旱性气候,但比第一阶段湿度可能稍有增加.这一总体干旱—半干旱气候格局及其变化总体与同期全球气候变化一致.
  • [1] Bocherens H, Friis E M, Mariotti A, et al. Carbon isotopic abundances in Mesozoic and Cenozoic fossil plants: Palaeoecological implications [J]. Lethaia, 1994, 26(4): 347-358.
    [2] 洪汉烈,于娜,薛惠娟,等. 临夏盆地晚更新世沉积物黏土矿物的特征及其古气候指示[J]. 现代地质,2007,21(2):406-414.[Hong Hanlie, Yu Na, Xue Huijuan, et al. Clay mineralogy and its palaeoclimatic indicator of the Late Pleistocene in Linxia Basin [J]. Geoscience, 2007, 21(2): 406-414.]
    [3] 李祥辉,徐宝亮,陈云华,等. 华北—东北南部地区中生代中晚期粘土矿物与古气候[J]. 地质学报,2008,82(5):683-691.[Li Xianghui, Xu Baoliang, Chen Yunhua, et al. Clay minerals of the Middle-Late Mesozoic mudrocks from North and Northeast China: Implications to paleoclimate and paleohighland [J]. Acta Geologica Sinica, 2008, 82(5): 683-691.]
    [4] 向芳,宋见春,罗来,等. 白垩纪早期陆相特殊沉积的分布特征及气候意义[J]. 地学前缘,2009,16(5):48-62.[Xiang Fang, Song Jianchun, Luo Lai, et al. Distribution characteristics and climate significance of continental special deposits in the Early Cretaceous [J]. Earth Science Frontiers, 2009, 16(5): 48-62.]
    [5] 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.[Liu Ling, Li Xianghui, Wang Yin, 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.]
    [6] 刘云,王宗哲. 广东南雄盆地白垩纪—第三系界线地层岩性特征及环境分析[J]. 地层学杂志,1986,10(3):190-203.[Liu Yun, Wang Zongzhe. The petrographic characters and environmental analysis of the Cretaceous-Tertiary boundary strata at the Nanxiong Basin Guangdong province [J]. Journal of Stratigraphy, 1986, 10(3): 190-203.]
    [7] 拉塞尔 D A,拉塞尔 D E,斯威特 A R. 关于南雄盆地K/T界线地层序列的几个问题[J]. 古脊椎动物学报,1993,31(2):139-145.[Russell D A, Russell D E, Sweet A R. The end of the dinosaurian era in the Nanxiong Basin [J]. Vertebrata Palasiatica, 1993, 31(2): 139-145.]
    [8] 陈丕基. 广东南雄上湖组叶肢介化石的发现—并论中国古新世陆相地层[J]. 古生物学报,1986,25(4):380-393.[Chen Piji. On the Chinese non-marine Paleocene from the new discovery of the conchostracan fauna of Nanxiong, Guangdong[J]. Acta Palaeontologica Sinica, 1986, 25(4): 380-393.]
    [9] 李思田. 中国东部及邻区中、新生代盆地演化及地球动力学背景[M]. 武汉:中国地质大学出版社,1997.[Li Sitian. Eastern China and Adjacent Areas in Mesozoic and Cenozoic Basin Evolution and Geochemical Dynamics Background [M]. Wuhan: China University of Geosciences Press, 1997.]
    [10] 舒良树,邓平,王彬,等. 南雄诸广地区晚中生代盆山演化的岩石化学、运动学与年代学制约[J]. 中国科学(D辑):地球科学,2004,34(1):1-13.[Shu Liangshu, Deng Ping, Wang Bin, et al. Late Mesozoic basin-range evolution of Nanxiong Zhuguang area: Constraint from petrochemistry, kinematics and geochronology [J]. Science China (Seri.D): Earth Sciences, 2004, 34(1): 1-13.]
    [11] 李佩贤,程政武,张志军,等. 广东南雄盆地的“南雄层”和“丹霞层”[J]. 地球学报,2007,28(2):181-189.[Li Peixian, Cheng Zhengwu, Zhang Zhijun, et al. The Nanxiong Bed and the Danxia Bed in the Nanxiong Basin of Guangdong province [J]. Acta Geoscientica Sinica, 2007, 28(2): 181-189.]
    [12] 张显球,林建南,李罡,等. 南雄盆地大塘白垩系—古近系界线剖面研究[J]. 地层学杂质,2006,30(4):327-340.[Zhang Xianqiu, Lin Jiannan, Li Gang, et al. Non-marine Cretaceous-Paleogene Boundary Section at Datang of Nanxiong, northern Guangdong [J]. Journal of Stratigraphy, 2006, 30(4): 327-340.]
    [13] 赵资奎,叶捷,李华梅,等. 广东省南雄盆地白垩系—第三系交界恐龙绝灭问题[J]. 古脊椎动物学报,1991,29(1):1-20.[Zhao Zikui, Ye Jie, Li Huamei, et al. Extinction of the dinosaurs across the Cretaceous-Tertiary boundary in Nanxiong Basin, Guangdong province [J]. Vertebrate Palasiatica, 1991, 29(1): 1-20.]
    [14] Ingersoll R V, Fullard T F, Ford R L,et al. The effect of grain size on detrital modes; a test of the Gazzi-Dickinson point-counting method [J]. Journal of Sedimentary Research, 1984, 54(1): 103-116.
    [15] 王成善,李祥辉. 沉积盆地分析原理与方法[M]. 北京:高等教育出版社,2003:92-98.[Wang Chengshan, Li Xianghui. Principles and Methods of Sedimentary Basin Analyses [M]. Beijing: Higher Education Press, 2003: 92-98.]
    [16] Liu Zhifei, Colin C, Huang Wei, et al. Climatic and tectonic controls on weathering in south China and Indochina Peninsula: Clay mineralogical and geochemical investigations from the Pearl, Red, and Mekong drainage basins [J]. Geochemistry, Geophysics, Geosystems, 2007, 8(5), doi:  10.1029/2006GC001490.
    [17] Holtzapffel T. LesMinéraux Argileux: Préparation, Analyse Diffractométrique et Détermination [M]. Société géologique du Nord, 1985.
    [18] Liu Zhifei, Zhao Yulong, Colin C, et al. Chemical weathering in Luzon, Philippines from clay mineralogy and major-element geochemistry of river sediments [J]. Applied Geochemistry, 2009, 24(11): 2195-2205.
    [19] Petschick R. Mac Diff version4.2.2. [Online]: http://servermac.geologie.un-frankfurt.de/Rainer.html, 2000.
    [20] Mikesell L R, Schaetzl R J, Velbel M A. Hornblende etching and quartz/feldspar ratios as weathering and soil development indicators in some Michigan soils [J]. Quaternary Research, 2004, 62(2): 162-171.
    [21] Wang Xulong, Miao Xiaodong. Weathering history indicated by the luminescence emissions in Chinese loess and paleosol [J]. Quaternary Science Reviews, 2006, 25(13/14): 1719-1726.
    [22] 杨作升,赵晓辉,乔淑卿,等. 长江和黄河入海沉积物不同粒级中长石/石英比值及化学风化程度评价[J]. 中国海洋大学学报,2008,38(2):244-250.[Yang Zuosheng, Zhao Xiaohui, Qiao Shuqing, et al. Feldspar/Quartz(F/O)Ratios as a chemical weathering intensity indicator in different grain size-fractions of sediments from the Changjiang and Huanghe Rivers to the seas [J]. Periodical of Ocean University of China, 2008, 38(2): 244-250.]
    [23] Singer A. The paleoclimatic interpretation of clay minerals in soils and weathering profiles [J]. Earth-Science Reviews, 1980, 15(4): 303-326.
    [24] Singer A. The paleoclimatic interpretation of clay minerals in sediments-a review [J]. Earth-Science Reviews, 1984, 21(4): 251-293.
    [25] Vanderaveroet P. Miocene to Pleistocene clay mineral sedimentation on the New Jersey shelf [J]. Oceanologica Acta, 2000, 23(1): 25-36.
    [26] Gingele F X, De Deckker P, Hillenbrand C D. Late Quaternary fluctuations of the Leeuwin Current and palaeoclimates on the adjacent land masses: clay mineral evidence [J]. Australian Journal of Earth Sciences, 2001, 48(6): 867-874.
    [27] Winkler A, Wolf-Welling T, Stattegger K,et al. Clay mineral sedimentation in high northern latitude deep-sea basins since the Middle Miocene(ODP Leg 151, NAAG) [J]. International Journal of Earth Sciences, 2002, 91(1): 133-148.
    [28] 蓝先洪. 粘土矿物作为古气候指标矿物的探讨[J]. 地质科技情报,1990,9(4):31-35.[Lan Xianhong. Clay minerals as an index of paleoclimate [J]. Geological Science and Technology Information, 1990, 9(4): 31-35.]
    [29] Keller W D. Environmental aspects of clay minerals [J]. Journal of Sedimentary Research, 1970, 40(3): 788-813.
    [30] Chamley H. Clay Sedimentology [M].Berlin: Springer-Verlag, 1989.
    [31] Esquevin J. Influence de la composition chimique des illites sur leur cristallinité [J].Bulletin du Centre de Recherches de Pau, Société Nationale des Pétroles d'Aquitaine, 1969, 3(1): 147-153.
    [32] Boero V, Premoli A, Melis P, et al. Influence of climate on the iron oxide mineralogy of Terra Rossa [J]. Clays and Clay Minerals, 1992, 40(1): 8-13.
    [33] 蓝先洪. 海洋沉积物中粘土矿物组合特征的古环境意义[J]. 海洋地质动态,2001,17(1):4-7.[Lan Xianhong. Marine sediments of clay mineral assemblages paleoenvironmental significance [J]. Marine Geology Development, 2001, 17(1): 4-7.]
    [34] 陈涛,王欢,张祖青,等. 粘土矿物对古气候指示作用浅析[J]. 岩石矿物学杂志,2003,22(4):416-420.[Chen Tao, Wang Huan, Zhang Zuqing, et al. Clay minerals as indicators of paleoclimate [J]. Acta Petrologica et Mineralogica, 2003, 22(4): 416-420.]
    [35] Thiry M. Palaeoclimatic interpretation of clay minerals in marine deposits: an outlook from the continental origin [J]. Earth-Science Reviews, 2000, 49(1/2/3/4): 201-221.
    [36] Keller G. The end-Cretaceous mass extinction in the marine realm: year 2000 assessment [J]. Planetary and Space Science, 2001, 49(8): 817-830.
    [37] 张显球,李罡. 广东南雄盆地罗佛寨群的介形类动物群[J]. 微体古生物学报,2008,25(1):44-77.[Zhang Xianqiu, Li Gang. Ostracod faunas from the Luofozhai Group in the Nanxiong Basin of Guangdong province, China[J]. Acta Micropalaeontologica Sinica, 2008, 25(1): 44-77.]
    [38] Erben H K, Ashraf A R, Boehm H, et al. Die Kreide/Tertiär-Grenze im Nanxiong-Becken: Kontinentalfazies, Südost China = The Cretaceous/Tertiary boundary in the Nanxiong-Basin: continental facies, SE-China [M].Stuttgart: F. Steiner,1995: 32.
    [39] 赵资奎,毛雪瑛,柴之芳,等. 广东南雄盆地白垩系—第三系交界恐龙蛋壳的铱丰度异常[J]. 中国科学(D 辑):地球科学,1998,28(5):425-430.[ Zhao Zikui, Mao Xueying, Chai Zhifang, et al. The dinosaur eggshells iridium abundance anomalies of the Cretaceous-Tertiary boundary strata in Nanxiong Basin, Guangdong province[J]. Science China (Seri. D): Earth Sciences, 1998, 28(5): 425-430.]
    [40] 赵资奎,严正. 广东南雄盆地白垩系—第三系界线剖面恐龙蛋壳稳定同位素记录:地层及古环境意义[J]. 中国科学(D 辑),2000,30(2):135-141.[Zhao Zikui, Yan Zheng. Nanxiong Cretaceous-Tertiary boundary section of dinosaur eggs stable isotope record: stratigraphic and paleoenvironmental significance[J].Science in China (Series D), 2000, 30(2): 135-141.]
    [41] Gradstein F M, Ogg J G, Kranendonk M. On thegeologic time scale 2008 [J]. Newsletters on Stratigraphy, 2008, 43(1): 5-13.
    [42] Clyde W C, Ting S, Snell K E,et al. New paleomagnetic and stable-isotope results from the Nanxiong Basin, China: Implications for the K/T boundary and the timing of Paleocene mammalian turnover [J]. The Journal of Geology, 2010, 118(2): 131-143.
    [43] Boucot A J,陈旭,Scotese C R,等. 显生宙全球古气候重建[M]. 北京:科学出版社,2009.[Boucot A J, Chen Xu, Scotese C R, et al. Phanerozoic Global Paleoclimate Reconstruction [M]. Beijing: Science Press, 2009.]] Mikesell L R, Schaetzl R J, Velbel M A. Hornblende etching and quartz/feldspar ratios as weathering and soil development indicators in some Michigan soils [J]. Quaternary Research, 2004, 62(2): 162-171.
    [44] Wang Xulong, Miao Xiaodong. Weathering history indicated by the luminescence emissions in Chinese loess and paleosol [J]. Quaternary Science Reviews, 2006, 25(13/14): 1719-1726.
    [45] 杨作升,赵晓辉,乔淑卿,等. 长江和黄河入海沉积物不同粒级中长石/石英比值及化学风化程度评价[J]. 中国海洋大学学报,2008,38(2): 244-250.[Yang Zuosheng, Zhao Xiaohui, Qiao Shuqing, et al. Feldspar/Quartz(F/O)Ratios as a chemical weathering intensity indicator in different grain size-fractions of sediments from the Changjiang and Huanghe Rivers to the seas [J]. Periodical of Ocean University of China, 2008, 38(2): 244-250.]
    [46] Singer A. The paleoclimatic interpretation of clay minerals in soils and weathering profiles [J]. Earth-Science Reviews, 1980, 15(4): 303-326.
    [47] Singer A. The paleoclimatic interpretation of clay minerals in sediments-a review [J]. Earth-Science Reviews, 1984, 21(4): 251-293.
    [48] Vanderaveroet P. Miocene to Pleistocene clay mineral sedimentation on the New Jersey shelf [J]. Oceanologica Acta, 2000, 23(1): 25-36.
    [49] Gingele F X, De Deckker P, Hillenbrand C D. Late Quaternary fluctuations of the Leeuwin Current and palaeoclimates on the adjacent land masses: clay mineral evidence [J]. Australian Journal of Earth Sciences, 2001, 48(6): 867-874.
    [50] Winkler A, Wolf-Welling T, Stattegger K, et al. Clay mineral sedimentation in high northern latitude deep-sea basins since the Middle Miocene(ODP Leg 151, NAAG) [J]. International Journal of Earth Sciences, 2002, 91(1): 133-148.
    [51] 蓝先洪. 粘土矿物作为古气候指标矿物的探讨[J]. 地质科技情报,1990,9(4): 31-35.[Lan Xianhong. Clay minerals as an index of paleoclimate [J]. Geological Science and Technology Information, 1990, 9(4): 31-35.]
    [52] Keller W D. Environmental aspects of clay minerals [J]. Journal of Sedimentary Research, 1970, 40(3): 788-813.
    [53] Chamley H. Clay Sedimentology [M]. Berlin: Springer-Verlag, 1989.
    [54] Esquevin J. Influence de la composition chimique des illites sur leur cristallinité [J]. Bulletin du Centre de Recherches de Pau, Société Nationale des Pétroles d'Aquitaine, 1969, 3(1): 147-153.
    [55] Boero V, Premoli A, Melis P, et al. Influence of climate on the iron oxidemineralogy of Terra Rossa [J]. Clays and Clay Minerals, 1992, 40(1): 8-13.
    [56] 蓝先洪. 海洋沉积物中粘土矿物组合特征的古环境意义[J]. 海洋地质动态,2001,17(1): 4-7.[Lan Xianhong. Marine sediments of clay mineral assemblages paleoenvironmental significance [J]. Marine Geology Development, 2001, 17(1): 4-7.]
    [57] 陈涛,王欢,张祖青,等. 粘土矿物对古气候指示作用浅析[J]. 岩石矿物学杂志,2003,22(4): 416-420.[Chen Tao, Wang Huan, Zhang Zuqing, et al. Clay minerals as indicators of paleoclimate [J]. Acta Petrologica et Mineralogica, 2003, 22(4): 416-420.]
    [58] Thiry M. Palaeoclimatic interpretation of clay minerals in marine deposits: an outlook from the continental origin [J]. Earth-Science Reviews, 2000, 49(1/2/3/4): 201-221.
    [59] Keller G. The end-Cretaceous mass extinction in the marine realm: year 2000 assessment [J]. Planetary and Space Science, 2001, 49(8): 817-830.
    [60] 张显球,李罡. 广东南雄盆地罗佛寨群的介形类动物群[J]. 微体古生物学报,2008,25(1): 44-77.[Zhang Xianqiu, Li Gang. Ostracod faunas from the Luofozhai Group in the Nanxiong Basin of Guangdong province, China[J]. Acta Micropalaeontologica Sinica, 2008, 25(1): 44-77.]
    [61] Erben H K, Ashraf A R, Boehm H, et al. Die Kreide/Tertiär-Grenze im Nanxiong-Becken: Kontinentalfazies, SüdostChina = The Cretaceous/Tertiary boundary in the Nanxiong-Basin: continental facies, SE-China [M]. Stuttgart: F. Steiner,1995: 32.
    [62] 赵资奎,毛雪瑛,柴之芳,等. 广东南雄盆地白垩系—第三系交界恐龙蛋壳的铱丰度异常[J]. 中国科学(D 辑),1998,28(5): 425-430.[ Zhao Zikui, Mao Xueying, Chai Zhifang, et al. The dinosaur eggshells iridium abundance anomalies of the Cretaceous-Tertiary Boundary strata in Nanxiong Basin, Guangdong province[J]. Science in China (Series D), 1998, 28(5): 425-430.]
    [63] 赵资奎,严正. 广东南雄盆地白垩系—第三系界线剖面恐龙蛋壳稳定同位素记录: 地层及古环境意义[J]. 中国科学(D 辑),2000,30(2): 135-141.[Zhao Zikui, Yan Zheng. Nanxiong Cretaceous-Tertiary boundary section of dinosaur eggs stable isotope record: stratigraphic and paleoenvironmental significance[J].Science in China (Series D), 2000, 30(2): 135-141.]
    [64] Gradstein F M, Ogg J G, Kranendonk M. On the geologic time scale 2008 [J]. Newsletters on Stratigraphy, 2008, 43(1): 5-13.
    [65] Clyde W C, Ting S, Snell K E, et al. New paleomagnetic and stable-isotope results from the Nanxiong Basin, China: Implications for the K/T boundary and the timing of paleocene mammalian turnover [J]. The Journal of Geology, 2010, 118(2): 131-143.
    [66] Boucot A J,陈旭,Scotese C R,等. 显生宙全球古气候重建[M]. 北京: 科学出版社,2009.[Boucot A J, Chen Xu, Scotese C R, et al. Phanerozoic Global Paleoclimate Reconstruction [M]. Beijing: Science Press, 2009.]
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  • 收稿日期:  2013-12-09
  • 修回日期:  2014-05-26
  • 刊出日期:  2015-02-10

目录

    南雄盆地晚白垩世—古新世陆源沉积组份变化的古气候指示

    doi: 10.14027/j.cnki.cjxb.2015.01.012
      基金项目:  国家自然科学基金项目(批准号:41372106)和国际重点基础研究发展计划“973”项目(编号:2012CB822003)联合资助
      作者简介:

      王尹 男 1985年出生 硕士 古气候与古土壤 E-mail: yin31721@qq.com

    • 中图分类号: P532

    摘要: 利用陆源沉积中的碎屑组份(泥岩中的碎屑黏土矿物种类和砂岩中砂、粉砂碎屑类型)相对含量变化,对广东北部和江西南部的南雄盆地晚白垩世—古新世古气候进行了分析.结果显示,砂岩碎屑组份含量气候指数(长石/石英比,F/Q)介于0.02~0.14之间;(碎屑)黏土矿物组合主要以伊利石为主,平均79%;伊利石结晶度指数与化学指数分别为0.25~0.39、0.31~0.7.进一步分析表明,研究区这一时期以干旱气候为主,存在暖湿气候间断,古气候演化可分为三个阶段:晚白垩世马斯特里赫特期以干旱—半干旱性气候为主,古新世丹尼期早期转变为相对湿热或与干旱—半干旱气候交替,古新世丹尼期晚期恢复到半干旱性气候,但比第一阶段湿度可能稍有增加.这一总体干旱—半干旱气候格局及其变化总体与同期全球气候变化一致.

    English Abstract

    王尹, 李祥辉, 周勇, 刘玲. 南雄盆地晚白垩世—古新世陆源沉积组份变化的古气候指示[J]. 沉积学报, 2015, 33(1): 116-123. doi: 10.14027/j.cnki.cjxb.2015.01.012
    引用本文: 王尹, 李祥辉, 周勇, 刘玲. 南雄盆地晚白垩世—古新世陆源沉积组份变化的古气候指示[J]. 沉积学报, 2015, 33(1): 116-123. doi: 10.14027/j.cnki.cjxb.2015.01.012
    WANG Yin, LI XiangHui, ZHOU Yong, LIU Ling. Paleoclimate Indication of Terrigenous Clastic Rock's Component during the Late Cretaceous-Early Paleocene in the Nanxiong Basin[J]. Acta Sedimentologica Sinica, 2015, 33(1): 116-123. doi: 10.14027/j.cnki.cjxb.2015.01.012
    Citation: WANG Yin, LI XiangHui, ZHOU Yong, LIU Ling. Paleoclimate Indication of Terrigenous Clastic Rock's Component during the Late Cretaceous-Early Paleocene in the Nanxiong Basin[J]. Acta Sedimentologica Sinica, 2015, 33(1): 116-123. doi: 10.14027/j.cnki.cjxb.2015.01.012
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