地球科学进展 ›› 2011, Vol. 26 ›› Issue (9): 1006 -1014. doi: 10.11867/j.issn.1001-8166.2011.09.1006

新学科·新技术·新发现 上一篇    

宁夏中奥陶统香山群徐家圈组内波、内潮汐沉积类型
李向东 1,2,何幼斌 2,张铭记 3,刘训 1,姚建新 1   
  1. 1.中国地质科学院地质研究所,北京 100037;2.长江大学地球科学学院,湖北 荆州 434023;3. 中国石油东方地球物理公司东部勘探事业部,陕西 西安 710021
  • 收稿日期:2010-08-24 修回日期:2011-08-16 出版日期:2011-09-10
  • 通讯作者: 李向东
  • 基金资助:

    国家自然科学基金项目“宁夏香山群内波、内潮汐沉积及其伴生沉积研究”(编号:40672071)和“鄂尔多斯盆地西缘中奥陶统深水牵引流沉积研究”(编号:41072086);中国地质科学院地质研究所基本科研项目“宁夏香山群复杂水动力条件下浊流沉积特征研究”(编号:J1110)资助.

Sedimentary Types of Internal-wave and Internal-tide Deposits of Middle Ordovician, Xujiajuan Formation, Xiangshan Group, Ningxia Autonomous Region, China

Li Xiangdong 1,2, He Youbin 2, Zhang Mingji 3, Liu Xun 1, Yao Jianxin 1   

  1. 1. Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China;2. School of Geoscience, Yangtze University, Jingzhou 434023, China;3. Changqing Division of East Exploration Department, BPG CNPC, Xi′an 710021, China
  • Received:2010-08-24 Revised:2011-08-16 Online:2011-09-10 Published:2011-10-10

内波、内潮汐沉积是深水沉积研究中一个非常年轻的研究领域,自发现到现在仅仅20年时间,对其沉积类型的研究目前尚未涉及。以宁夏香山群徐家圈组中的内波、内潮汐沉积为对象,详细描述了深水环境中形成的双向交错层理、单向交错层理、复合流层理及具有波状纹层、束状纹层和交错纹层透镜体的交错层理,并探讨了其成因机制,识别出了短周期内波沉积。在此基础之上,结合已有的内波、内潮汐沉积鉴别标志,从沉积构造的角度对内波、内潮汐沉积类型进行了探讨。将内波、内潮汐沉积分为短周期内波沉积、内潮汐沉积和叠加内波沉积。鉴于内潮汐形成机制的独特性和海洋物理学中内波的研究现状,三者仍统称为内波、内潮汐沉积。

The study of internal-wave and internal-tide deposits is a very young research field with twenty years of history in the deep-water deposition, and there is no study on its sedimentary types. Here, we forcus on the internal-wave and internal-tide deposits developed in Xujiajuan Formation, Xiangshan Group, Ningxia Autonomous Region and describe related sedimentary structures in detail. We interpret combined-flow-ripple lamination and the cross beddings with undulatory laminations, offshooting laminations and cross-laminated lenses as combined-flow and oscillatory flow generated by short-period internal waves respectively. According to these new interpretations and the interpretations of deep-water bidirectional cross-beddings and unidirectional crossbeddings in literatures, we attribute internal-wave and internal-tide deposits to short-period internal-wave deposits, internal-tide deposits and interaction internal-wave deposits. Here, we use internal-wave and internal-tide deposits instead of internal-wave deposits because of the special origin and research status of internal tides.

中图分类号: 

[1] Lafond E C. Internal waves[M]Fairbridge R W ed.The Encyclopedia of Oceangraphy.New York: Reinhold, 1966:402-408.
[2] Rattray M.On the coastal generation of internal tides[J].Tellus, 1960, 12(1): 54-62.
[3] Gao Zhenzhong, Eriksson K A.Internal-tide deposits in an Ordovician submarine channel:Previously unrecognized facies? [J].Geology, 1991, 19 (7): 734-737.
[4] Gao Zhenzhong, He Youbin, Li Xiangdong.Study of internal-wave and internal-tide deposits in the ancient stratigraphical record from China [J].Journal of Paleogeography, 2010, 12(5): 515-527.[高振中,何幼斌,李向东.中国地层记录中内波、内潮汐沉积研究[J].古地理学报,2010,12(5):515-527.]
[5] Gao Zhenzhong, Eriksson K A, He Youbin, et al.Deep-water Traction Current Deposits—A Study of Internal Tides, Internal Waves, Contour Currents and Their Deposits [M]. Beijing and New York: Science Press, Utrecht and Tokyo: VSP, 1998.
[6] He Youbin, Gao Zhenzhong.The characteristics and recognition of internal-tide and internal-wave deposits [J].Chinese Science Bulletin, 1999, 44(7): 582-589.
[7] He Youbin, Gao Zhenzhong, Luo Jinxiong, et al.Characteristics of internal-wave and internal-tide deposits and their hydrocarbon potential [J].Petroleum Science, 2008, 5(1): 37-43.
[8] He Youbin, Luo Shunshe, Gao Zhenzhong.Current situation and advance of internal-wave and internal-tide deposit study [J].Journal of Jianghan Petroleum Institute, 2004, 26(1): 5-10.[何幼斌,罗顺社,高振中.内波、内潮汐沉积研究现状与进展[J].江汉石油学院学报,2004,26 (1): 5-10.]
[9] Gao Zhenzhong, He Youbin, Liu Chengxin, et al.History, status and prospect of study on deep-water traction current deposits [J].Journal of Palaeogeography, 2006, 8(3): 331-338.[高振中,何幼斌,刘成鑫,等.深水牵引流沉积的研究历程、现状与前景[J].古地理学报,2006,8(3):331-338.][10] Zhang Xingyang, He Youbin, Luo Shunshe, et al.Deep-water sediment waves formed by internal waves [J].Journal of Palaeogeography, 2002, 4(1): 83-89.[张兴阳,何幼斌,罗顺社,等.内波单独作用形成的深水沉积物波[J].古地理学报,2002,4(1): 83-89.]
[11] Zhang Xingyang, Gao Zhenzhong, Yao Xuegen.Internal-wave deposits in the north-eastern Rockall Trough, North Atlantic Ocean-Reinterpretation of deep-water sediment waves formation [J].Acta Sedimentologica Sinica, 1999, 17(3): 80-83.[张兴阳,高振中,姚雪根.北大西洋洛克尔海槽东北部内波沉积——深水大型沉积物波成因的再解释[J].沉积学报,1999,17(3): 464-472.]
[12] Wang Qingchun, Bao Zhidong, He Ping.The generational mechanism of orientating sedimentary structure by internal-waves [J].Acta Sedimentologica Sinica, 2005, 23(2): 255-259.[王青春,鲍志东,贺萍.内波沉积中指向沉积构造的形成机理[J].沉积学报,2005,23(2):255-259.]
[13] He Youbin, Luo Jinxiong, Xin Changjin, et al.Characteristics and origins of deep-sea large-scale sediment wave[J].Journal of China University of Geosciences, 2007, 18(S): 305-307.
[14] Gao Ping, He Youbin.Status and prospect of study on deep-sea large-scale sediment waves [J].Marine Sciences, 2009, 33 (5): 92-97.[高平,何幼斌.深水大型沉积物波的研究现状与展望[J].海洋科学,2009,33 (5):92-97.]
[15] Tong Yanming, He Youbin, Zhu Guanghui.Classification of internal-wave and internal-tide deposits in deep-water and significance to petroleum prospecting [J].Marine Origin Petroleum Geology, 2006, 12(2): 39-45.[佟彦明,何幼斌,朱光辉.深水内波、内潮汐沉积类型及其油气意义[J].海相油气地质,2006,12 (2): 39-45.]
[16] He Youbin, Gao Zhenzhong, Luo Jinxiong, et al.Characteristics of internal-wave and internal-tide deposits and their hydrocarbon potential[J].Petroleum Science, 2008, 5 (1): 37-43.
[17] Wang Zhenfan, Zheng Zhaochang.The age of the Xiangshan Group in Ningxia[J].Regional Geology of China, 1998, 17 (1): 69-73.[王振藩,郑昭昌.宁夏香山群的时代探讨[J].中国区域地质,1998,17(1):69-73.]
[18] Zhang Kang.Discussion on the geological age of the Xiangshan Group in the Ordos Basin [J].Experimental Petroleum Geology, 1993, 15(3): 309-316.[张抗.香山群时代讨论[J].石油实验地质,1993,15(3):309-316.]
[19] Li Tianbin.Re-discussion of Stratigraphic age of Xiangshan Group, Ningxia[J].Northwestern Geology, 1997, 18 (2): 1-9.[李天斌.宁夏香山群地层时代的再讨论[J].西北地质,1997,18(2):1-9.]
[20] Li Xiangdong, He Youbin, Zheng Zhaochang, et al.Deep-water combined-flow sedimentary structures in Xujiajuan Formation of Xiangshan Group, Ningxia [J].Acta Geologica Sinica, 2010, 84(2): 221-232.[李向东,何幼斌,郑昭昌,等.宁夏香山群徐家圈组发现深水复合流沉积构造[J].地质学报,2010,84 (2):221-232.]
[21] Li Xiangdong, He Youbin, Wang Dan, et al.Analysis on Palaeocurrent in the Xujiajuan Formation, Xiangshan Group, Middle Ordovicaian, in southern Helan Mountains [J].Geological Review, 2009, 55(5): 653-662.[李向东,何幼斌,王丹,等.贺兰山以南中奥陶统香山群徐家圈组古水流分析[J].地质论评,2009,55(5):653-662.]
[22] Li Xiangdong, He Youbin, Wang Dan, et al.Internal-wave and internal-tide deposits of the Middle Ordovicaian Xiangshan Group Xujiajuan Formation, Ningxia [J].Journal of Palaeogeography, 2009, 11(5): 513-523.[李向东,何幼斌,王丹,等.宁夏中奥陶统香山群徐家圈组内波内潮汐沉积[J].古地理学报,2009,11(5):513-523.]
[23] Allen P A.Wave-generated structures in the Devonian lacustrine sediments of south-east Shetland and ancient wave conditions [J].Sedimentology, 1981, 28(3): 369-379.
[24] Bagnold R A.Motion of waves in shallow water: Interactions between waves and bottoms [J].Proceedings of the Royal Society A, 1946, 187(1): 1-15.[25] Raafde J F M, Boersma J R, Gelder V A.Wave-generated structures and sequences from a shallow marine succession, Lower Carboniferous, County Cork, Ireland [J].Sedimentology, 1977, 24(4): 451-483.
[26] Cotter E.Depositional setting and cyclic development of the lower part of the Witteberg Group (Mid-to Upper Devonian), Cape Supergroup, Western Cape, South Africa [J].South African Journal of Geology, 2000, 103(1): 1-14.
[27] Dumas S, Arnott R W C, Southard J B.Experiments on oscillatory-flow and combined-flow bed forms: Implications for interpreting parts of the shallow-marine sedimentary record [J].Journal of Sedimentary Research, 2005, 75(3): 501-513.
[28] Arnott R W, Southard J B.Exploratory flow-duct experiments on combined-flow bed configurations and some implications for interpreting storm-event stratification [J].Journal of Sedimentary Petrology, 1990, 60(2): 211-219.
[29] Lamb M P, Myrow P M, Lukens C, et al.Deposits from wave-influenced turbidity currents: Pennsylvanian Minturn Formation, Colorado, USA [J].Journal of Sedimentary Research, 2008, 78(7): 480-498.
[30] Myrow P M, Fischer W, Goodge J W.Wave-modified turbidites: Combined-flow shoreline and shelf deposits, Cambrian, Antarctica [J].Journal of Sedimentary Research, 2002, 72(5): 641-656.
[31] Lin Mian, Yuan Zhida.Investigation of characteristics of fluid field over wavy beds under oscillatory flow [J].Chinese Journal of Geophysics, 2005, 48 (6): 1 466-1 474.[林缅,袁志达.振荡流作用下波状底床上流场特性的实验研究[J].地球物理学报,2005,48 (6):1 466-1 474.]
[32] Zedler E A, Street R L.Sediment transport over ripples in oscillatory flow[J].Journal of Hydraulic Engineering,2006, 132(2): 180-193.
[33] Ribberink J S, Werf J J, O′Donoghue T.Sand motion induced by oscillatory flows: Sheet flow and vortex ripples[M]Geurts B J,et al,eds.Particle Laden Flow: From Geophysical to Kolmogorov Scales.Verlgg:Springer, 2007:3-14.
[34] Yokokawa M, Masuda F, Endo N.Sand particle movement on migrating combined-flow ripples[J].Journal of Sedimentary Research,1995,65(1):40-44.[35] Dumas S, Arnott R W C, Southard J B.Experiments on oscillatory-flow and combined-flow bed forms: Implications for interpreting parts of the shallow-marine sedimentary record [J].Journal of Sedimentary Research, 2005, 75 (3): 501-513.
[36] Du Tao, Wu Wei, Fang Xinhua.The generation and distribution of ocean internal waves [J].Marine Sciences,2001,25(4): 25-28.[杜涛,吴巍,方欣华.海洋内波的产生与分布[J].海洋科学,2001,25(4):25-28.]
[37] Gao Zhenzhong, He Youbin, Li Jianming, et al.The first internal-tide deposits found in China [J].Chinese Science Bulletin, 1997, 42(13): 1 113-1 117.[38] He Youbin, Gao Zhenzhong, Li Jianming, et al.Internal-tide deposits of the late Ordovician in Tonglu, Zhejiang [J].Acta Sedimentologica Sinica, 1998, 16(1): 1-7.[何幼斌,高振中,李建明,等.浙江桐庐晚奥陶世内潮汐沉积[J].沉积学报,1998,16 (1):1-7.]
[39] Gao Zhenzhong,He Youbin,Zhang Xingyang,et al.Internal-wave and internal-tide deposits of the middle-upper Ordovician in the center Tarim Basin[J].Acta Sedimentologica Sinica, 2000,18(3):400-407.[高振中,何幼斌,张兴阳,等.塔中地区中晚奥陶世内波、内潮汐沉积[J].沉积学报,2000,18(3):400-407.]
[40] He Youbin, Gao Zhenzhong, Zhang Xingyang, et al.Internal-tide deposits of the middle and upper Ordovician in Well TZ32, Tarim Basin [J].Journal of Palaeogeography, 2003,5(4): 414-425.[何幼斌,高振中,张兴阳,等.塔里木盆地塔中32井中上奥陶统内潮汐沉积[J].古地理学报,2003,5(4):414-425.]
[41] Jin Huijuan, Li Yuci, Fang Guoqing.Internal-wave and internal-tide deposits in the palaeostratigraphic record of the western Qinling Mountains and their origin [J].Acta Sedimentologica Sinica, 2002,20(1):80-83.[晋慧娟,李育慈,方国庆.西秦岭古代地层记录中内波、内潮汐沉积及其成因解释[J].沉积学报,2002,20(1):80-83.]
[42] Guo Jianqiu, Zhang Xionghua, Zhang Zejun.Internal-wave and internal-tide deposits of Xiushui Formation of Shuangqiaoshan Group in Middle Proterozoic Era in Xiushui area, Jiangxi province[J].Geological Science and Technology Information, 2003,22(1): 47-51.[郭建秋,张雄华,章泽军.江西修水地区中元古界双桥山群修水组内波内潮汐沉积[J].地质科技情报,2003,22(1):47-51.]
[43] Guo Jianqiu, Zhang Xionghua, Zhang Zejun, et al.First discovery of internal-wave and internal-tide deposits from the Precambrian in Northwestern Jiangxi [J].Chinese Journal of Geology, 2004,39(3): 329-338.[郭建秋,张雄华,章泽军,等.赣西北前寒武系首次发现内波内潮汐沉积[J].地质科学,2004,39(3):329-338.]
[44] Li Jianming, Wang Hua, He Youbin, et al.Internal-tide deposits of Upper Ordovician flysch in Lin′an area of Zhejing province[J].Journal of Oil and Gas Technology, 2005,27(1): 1-4. [李建明,王华,何幼斌,等.浙江临安上奥陶统复理石中的内潮汐沉积[J].石油天然气学报,2005,27(1):1-4.]
[45] Li Jianming, He Youbin, Gao Zhenzhong, et al.Internal-tide deposits and paragenetic sedimentary characteristics of Precambrian in Banbianshan of Taojiang area of Hunan province[J].Journal of Oil and Gas Technology, 2005,27(5): 545-547.[李建明,何幼斌,高振中,等.湖南桃江半边山前寒武纪内潮汐沉积及其共生沉积特征[J].石油天然气学报,2005,27(5):545-547.]
[46] He Youbin, Gao Zhenzhong, Guo Chengxian, et al.Study on internal-wave and internal-tide deposits of the third member of the lower Cambrian Balang Formation at Yangjiaping, Shimen [J].Geology in China, 2005,32(1): 62-69.[何幼斌,高振中,郭成贤,等.石门杨家坪下寒武统杷榔组三段内波和内潮汐沉积研究[J].中国地质,2005,32(1):62-69.]
[47] He Youbin, Gao Zhenzhong, Luo Shunshe, et al.Discovery of internal-tide deposits from the third member of Pingliang Formation in Longxian area, Shaanxi province[J].Journal of Oil and Gas Technology, 2007, 29(4): 28-33.[何幼斌,高振中,罗顺社,等.陕西陇县地区平凉组三段发现内潮汐沉积[J].石油天然气学报,2007,29(4): 28-33.]
[48] Ding Haijun, Meng Xianghua,Ge Ming.Internal tide and internal wave deposites in flysch of Miboshan Formation [J].Geology of Anhui, 2008, 18(4): 241-247. [丁海军,孟祥化,葛铭.米钵山组复理石中的内潮汐沉积[J].安徽地质,2008,18(4):241-247.]
[49] Emery K O, Gunnerson C G.Internal swash and surf[J].Proceedings of the National Academy of Sciences, USA,1973, 70(8): 2 379-2 380.

[1] 李向东,陈海燕,陈洪达. 鄂尔多斯盆地西缘桌子山地区上奥陶统拉什仲组深水复合流沉积[J]. 地球科学进展, 2019, 34(12): 1301-1315.
[2] 郭荣涛. 硅质碎屑岩中的微生物席相关构造——联接现代与过去的纽带[J]. 地球科学进展, 2013, 28(4): 467-476.
阅读次数
全文


摘要