Review of sedimentation types and relevant concepts in mountain provenance
Zhong Dakang1, 2
1 State Key Laboratory of Petroleum Resource and Prospecting,China University of Petroleum(Beijing),Beijing 102249; 2 College of Geosciences,China University of Petroleum(Beijing),Beijing 102249
Abstract：By systematically reviewing the research results of sedimentation types in exhumation provenance during recent decades to centuries at home and abroad,combined field study in modern sediments of Quaternary,based on whether sediments transport,transportation mechanism,sedimentation location,gradient and landform, etc., the sedimentation types in exhumation provenance can be divided into eluvium,deluvium,colluvium,fluvial deposits in mountain-girt valley,pluvium,alluvium,etc. Various types have obvious differences in basic conception and connotation.Eluvium is sedimentation in-situ of the parent rock weathering product on the gentle landform(<3°). Deluvium is the deposits formed from parent rock weathering by sliding or rolling to the foot of the slopes under the impact of overland flow or gravity on the tilt landform (>3°,but no more than 30°). Colluvium is the deposits formed only under the impact of gravity by sliding or rolling to the foot of the slopes in the way of caving or fall or collapse on the steep landform (>30°). Fluvial deposits in mountain-girt valley form when eluvium,deluvium,colluvium are carried to valley or channel in mountains by overland flow. Pluvium forms during flood period when plenty of parent rock weathering products carried by intermountain flood current are located in mountain pass. Alluvium forms during normal river flow period when plenty of parent rock weathering products carried by intermountain flood current are located in mountain pass.In addition,gravity flow deposits such as landslide,slump,debris flow, etc., also exist in exhumation provenance.
[1] 奥勃鲁切夫 B A. 1929. 野外调查手册. [Oblomov B A. 1929. Field Survey Manual] [2] 鲍志东,郑秀娟. 2013. 冲积扇. 冯增昭主编. 中国沉积学(第二版). 北京: 石油工业出版社, 619-651. [Bao Z D, Zheng X J. 2013. Alluvial Fans. Feng Z Z(ed). 2013. Sedimentology of China (The second edition). Beijing: Petroleum Industry Press, 619-651] [3] 蔡雄飞,廖计华,蔡海磊,郑有业. 2007. 第四系冲、洪积物的识别标志和研究意义. 海洋地质动态,(1):10-12. [Cai X F,Liao J H,Cai H L, Zheng Y Y. 2007. The identification and research significance of alluvial and diluvium deposits in Quaternary. Marine Geology Letters,(1):10-12] [4] 蔡雄飞,智铎强,罗中杰,吴义布. 2011. 内蒙古固阳盆地东北缘更新统洪积物地层的发现及研究意义. 地层学杂志,35(2):172-178. [Cai X F,Zhi Z Q,Luo Z J, Wu Y B. 2011. Discovery and significance of Pleistocene alluvial deposition in Guyang Basin northeast margin,inner Mongolia. Journal of Stratigraphy,35(2):172-178] [5] 曹伯勋. 1995. 地貌学与第四纪地质学. 武汉:中国地质大学出版社. [Cai B X. 1995. Geomorphology and Quaternary Geology. Wuhan: China University of Geosciences Press] [6] 冯增昭. 1982. 沉积岩石学. 北京: 石油工业出版社. [Feng Z Z. 1982. Sedimentology. Beijing: Petroleum Industry Press] [7] 格拉西莫夫H Ⅱ. 1955. 中国的黄土及其成因. 北京: 地质出版社. [Gerasimov H Ⅱ. 1955. China’s Loess and Its Causes. Beijing: Geological Publishing House] [8] 尼古拉耶夫H N. 1958. 关于研究中国新构造的若干理论和方法问题. 北京: 科学出版社. [Nikolaev H N. 1958. Some Theoretical and Methodological Issues Concerning China’s New Research Structure. Beijing: Science Press] [9] 郭建华,朱美衡,杨申谷,刘辰生. 2003. 辽河盆地曙一区馆陶组湿地冲积扇沉积. 沉积学报,21(3):367-372. [Guo J H,Zhu M H,Yang S G, Liu C S. 2003. Wet alluvial fan sedimentary in the Guantao Formation of Shuyi area. Acta Sedimentologica Sinica,21(3):367-372] [10] 何丙辉,刘立志. 2007. 遂宁组紫色页岩崩解过程及坡积物特征研究. 西南大学学报(自然科学版),(1):48-52. [He B H,Liu L Z. 2007. Study on the cracking process of purple shale and the characteristics of alluvial purple soil developed from Suining Group. Journal of Southwest University(Nature Science),(1):48-52] [11] 纪洪磊. 2010. 滹沱河冲积扇冲洪积物光释光测年及其晚更新世以来气候演化释光年代学. 中国地质科学院. [Ji H L. 2010. OSL dating of alluvial sediments of the Hutuo-river alluvial fan and the luminescence chronology of climate evolution since late Pleistocene. Chinese Academy of Geological Sciences] [12] 赖内克H E,辛格I B. 1979. 陆源碎屑沉积环境. 北京: 石油工业出版社. [Reinecke H E,Synge I B. 1979. Terrigenous Clastic Sedimentary Environment. Beijing: Petroleum Industry Press] [13] 李新坡. 2007. 中国北方地区冲积扇地貌发育特征与影响因素分析. 北京大学. [Li X P. 2007. Geomorphology and affecting factors analysis of alluvial fans in North China.Peking University] [14] 李新坡,莫多闻,朱忠礼. 2006. 侯马盆地冲积扇及其流域地貌发育规律. 地理学报,61(3):241-248. [Li X P,Mo D W,Zhu Z L. 2006. Developments of alluvial fans and their catchments in Houma Basin. Acta Geographica Sinica,61(3):241-248] [15] 李新坡,莫多闻,朱忠礼,马元旭,刘运明. 2007. 一个片流过程控制的冲积扇: 太原盆地风峪沟冲积扇. 北京大学学报(自然科学版),43(4):560-566. [Li X P,Mo D W,Zhu Z L, Ma Y X, Liu Y M. 2007. A sheetflood-dominated alluvial fan-FengYG alluvilal fan,Taiyuan Basin. Acta Scientiarum Naturalium Universitatis Pekinensis,43(4):560-566] [16] 刘宝珺. 1980. 沉积岩石学. 北京:地质出版社. [Liu B J. 1980. Sedimentology. Beijing:Geological Publishing House] [17] 刘宝珺,曾允孚. 1985. 岩相古地理基础和工作方法. 北京: 地质出版社. [Liu B J,Zeng R F. 1985. The Basis and Working Methods of Lithofacies Palaeogeography. Beijing: Geological Publishing House] [18] 刘汉元,李远鄂. 1984. 湘江流域若干重金属元素在岩石、残坡积物及水中的背景值研究. 环境科学学报,(1):17-32. [Liu H Y,Li Y E. 1984. Background values of some metals in rocks,soil and water in Xiang jiang Basin. Acta Scientiae Circumstantiae,(1):17-32] [19] 刘疆,白志强. 2009. 广西横县六景古近纪冲积物研究. 北京大学学报(自然科学版),45(1):97-103. [Liu J,Bai Z Q. 2009. Study on Paleogene alluvial fan at Liujing,Guangxi,South China. Acta Scientiarum Naturalium Universitatis Pekinensis,45(1):97-103] [20] 鲁欣. 1955. 沉积岩石学原理. 北京: 地质出版社. [Рухин Л В. 1995. The Principle of Sedimentology. Beijing: Geological Publishing House] [21] 马玉凤,李双权,潘星慧. 2015. 黄河冲积扇发育研究述评. 地理学报,70(1):49-62. [Ma Y F,Li S Q,Pan X H. 2015. A review on development of the Yellow River alluvial fan. Acta Geographica Sinica,70(1):49-62] [22] 莫多闻,朱忠礼,万林义. 1999. 贺兰山东麓冲积扇发育特征. 北京大学学报(自然科学版),35(6):91-98. [Mo D W,Zhu Z L,Wan L Y. 1999. The alluvial fans along the eastern foot of Helan Moutain. Acta Scientiarum Naturalium Universitatis Pekinensis,35(6):91-98] [23] 南京大学地理系地貌教研组. 1961. 第四纪地质学. 北京: 人民教育出版社. [Geography Landscape Research Group of Nanjing University. 1961. Quaternary Geology. Beijing: People’s Educational Publishing House] [24] 钱宁,张仁,周志德. 1987. 河床演变学. 北京: 科学出版社. [Qian N,Zhang R,Zhou Z D. 1987. Riverbed Evolution. Beijing: Science Press] [25] 时志强,韩永林,赵俊兴. 2002. 鄂尔多斯盆地早侏罗世富县期冲积扇沉积. 成都理工学院学报,29(4):390-393. [Shi Z Q,Han Y L,Zhao J X. 2002. Fans at the early Jurassic Fuxian Stage in Ordos Basin. Journal of Chengdu University of Tecchnology,29(4):390-393] [26] 田建梅,李有利,司苏沛,吕胜华,王怡然. 2013. 中条山北麓中段洪积扇上全新世断层陡坎的发现及其新构造意义. 北京大学学报(自然科学版),49(6):986-992. [Tian J M,Li Y L,Si S P, Lü S H, Wang Y R. 2013. Discovery and Neotectonic significance of fault scarps on alluvial fans in the Middle of northern piedmont of the Zhongtiao Mountains. Acta Scientiarum Naturalium Universitatis Pekinensis,49(6):986-992] [27] 田明中,程捷. 2009. 第四纪地质学与地貌学. 北京: 地质出版社. [Tian M Z,Cheng J. 2009. The Quaternary Geology and Geomorphology. Beijing: Geological Publishing House] [28] 王红亚,霍豫英,吴秀芹,蔡运龙. 2006. 贵州石板桥水库沉积物的矿物磁性特征及其土壤侵蚀意义. 地理研究,25(5):865-876. [Wang H Y,Huo Y Y,Wu X Q, Cai Y L. 2006. Mineral magnetic charachteristics of sediments from Shibanqiao Reservoir,Guanling County,Guizhou Province and their implications on soil erosion. Geographical Research, 25(5):865-876] [29] 王良忱,张金亮. 1996. 沉积环境和沉积相. 北京: 石油工业出版社. [Wang L S,Zhang J L. 1996. Sedimentary Environment and Sedimentary Facies. Beijing: Petroleum Industry Press] [30] 王萍,卢演俦,丁国瑜,陈杰,Karl￣heinz Wyrwoll. 2004. 甘肃疏勒河冲积扇发育特征及其对构造活动的响应. 第四纪研究,24(1):74-81. [Wang P,Lu Y C,Ding G Y, Chen J, Wyrwoll K H. 2004. Response of the development of the Shule River alluvial fan to tectonic activity. Quaternary Sciences,24(1):74-81] [31] 王清,唐大雄,张庆云,赵继增. 1991. 中国东部花岗岩残积土物质成分和结构特征的研究. 长春地质学院学报,21(1):73-81. [Wang Q,Tang D X,Zhang Q Y, Zhao J Z. 1991. A study on the structure and composition of granite residual soil in the eastern China. Journal of Changchun University of Earth Science,21(1):73-81] [32] 王数,东野光亮. 2004. 地质学与地貌学. 北京: 中国农业大学出版社. [Wang S,Dongye G L. 2004. Geology and Geomorphology. Beijing: China Agricultural University Press] [33] 王艳清,李森明,田翔,杨体源. 2013. 柴达木盆地西部地区古—始新世残—坡积物的判别及意义. 中国地质,40(4):1307-1313. [Wang Y Q,Li S M,Tian X, Yang T Y. 2013. Identification and significance of the Paleocene-Eocene residual-slope sediments in western Qaidam Basin. Geology in China,40(4):1307-1313] [34] 王勇,钟建华,王志坤,段宏亮,连承波. 2007. 柴达木盆地西北缘现代冲积扇沉积特征及石油地质意义. 地质论评,53(6):791-796. [Wang Y,Zhong J H,Wang Z K, Duan H L, Lian C B. 2007. Sedimentary characteristics of modern alluvial fans in the northwest margin of the Qaidam Basin and their significance in petroleum geology. Geological Review,53(6):791-796] [35] 王运生,孙书勤,李永昭. 2007. 地貌学与第四纪地质学简明教程. 成都:四川大学出版社. [Wang Y S,Sun S Q,Li Y Z. 2007. The Introductory Tutorial of Geomorphology and Quaternary Geology. Chengdu:Sichuan University Press] [36] 吴崇筠,赵澄林,郝石生. 1982. 油区岩相古地理. 石油工业部勘探培训中心. [Wu C Y,Zhao C L,Hao S S. 1982. Lithofacies Palaeogeography of Oilfields. Training Centre of Petroleum Exploration Industry] [37] 吴崇筠,薛叔浩. 1992. 中国含油气盆地沉积学. 北京: 石油工业出版社. [Wu C Y,Xu S H. 1992. The Sedimentology of Oil and Gas in China. Beijing: Petroleum Industry Press] [38] 谢宇平. 1994. 第四纪地质学与地貌学. 北京: 地质出版社. [Xie Y P. 1994. The Quaternary Geology and Geomorphology. Beijing: Geological Publishing House] [39] 许清海,吴忱,孟令尧,王子惠,阳小兰,姚祖驹. 1994. 华北平原不同地貌单元冲积物孢粉组合特征. 科学通报,39(19):1792-1795. [Xu Q H,Wu S,Meng L R, Wang Z H, Yang X L, Yao Z J. 1994. The pollen assemblages in different geomorphic units of North China. Chinese Science Bulletin,39(19):1792-1795] [40] 雅科夫列夫C A. 1958. 第四纪沉积的研究与地质测量方法指南. 北京: 地质出版社. [Yakovlev C A. 1958. The Quaternary Sedimentary Research and Geological Measurement Guide. Beijing: Geological Publishing House] [41] 严钦尚,曾昭璇. 1985. 地貌学. 北京: 高等教育出版社. [Yan Q S,Zeng Z X. 1985. Geomorphology. Beijing: Higher Education Press] [42] 杨东伟,关平,李建民. 1990. 英汉沉积学解释词典. 北京: 北京大学出版社. [Yang D W,Guan P,Li J M. 1990. An English-Chinese Dictionary of Sedimentology. Beijing: Peking University Press] [43] 杨景春. 1984. 地貌学教程. 北京:北京大学出版社. [Yang J C. 1984. Course of Geomorphology. Beijing: Peking University Press] [44] 杨景春. 2001. 地貌学原理. 北京: 北京大学出版社. [Yang J C. 2001. Principal of Geomorphology. Beijing: Peking University Press] [45] 杨景春. 2005. 地貌学原理. 北京: 北京大学出版社. [Yang J C. 2005. Principal of Geomorphology. Beijing: Peking University Press] [46] 杨景春. 2012. 地貌学原理. 北京: 北京大学出版社. [Yang J C. 2012. Principal of Geomorphology. Beijing: Peking University Press] [47] 于兴河. 2002. 碎屑岩系油气储集层沉积学. 北京: 石油工业出版社. [Yu X H. 2002. Sedimentology of Clastic Rock Series in Oil and Gas Reservoirs. Beijing: Petroleum Industry Press] [48] 于兴河. 2008. 碎屑岩系油气储集层沉积学(第二版). 北京: 石油工业出版社. [Yu X H. 2008. Sedimentology of Clastic Rock Series in Oil and Gas Reservoirs(The second edition). Beijing: Petroleum Industry Press] [49] 余宽宏,金振奎,李桂仔,何苗,郭秀娟,杨婷. 2015. 准噶尔盆地克拉玛依油田三叠系克下组洪积砾岩特征及洪积扇演化. 古地理学报,17(2):143-159. [Yu K H,Jin Z K,Li G Z, He M, Guo X J, Yan T. 2015. Conglomerate characteristics and alluvial fan evolution of the Triassic Lower Karamay Formation in Karamay Oilfield,Junggar Basin. Journal of Palaeogeography(Chinese Edition),17(2):143-159] [50] 曾朋. 2012. 花岗岩残积土的压实特性及崩解特性研究. 华南理工大学. [Zeng P. 2012. The study of compaction and disintegration characteristics of the granite residual soil. South China University of Technology] [51] 张纪易. 1980. 克拉玛依洪积扇粗碎屑储集体. 新疆石油地质,1(1):33-53. [Zhang J Y. 1980. Pluvial fan coarse clastic reservoir in Karamay. Xinjiang Petroleum Geolgoy,1(1):33-53] [52] 张纪易. 1985. 粗碎屑洪积扇的某些沉积特征和微相划分. 沉积学报,3(3):75-85. [Zhang J Y. 1985. Some depositional characteristics and microfacies subdivision of coarse clastic alluvial fans. Acta Sedimentologica Sinica,3(3):75-85] [53] 张纪易. 1993. 冲积扇. 冯增昭主编. 中国沉积学. 北京: 石油工业出版社, 347-371. [Zhang J Y. 1993. Alluvial Fans. Feng Z Z(ed). Sedimentology of China. Beijing: Petroleum Industry Press, 347-371] [54] 张梅,陈艺鑫,银森录,张敬春,李川川,刘耕年. 2011. 格尔木河小干沟坡积沉积特征与古环境重建. 干旱区地理,34(6):890-903. [Zhang M,Chen Y X,Yin S L, Zhang J C, Li C C, Liu G N. 2011. Sedimental features and paleo-environment reconstruction of the slope deposit at Xiaoganguo of the Golmud River. Arid Land Geography,34(6):890-903] [55] 张抒. 2009. 广州地区花岗岩残积土崩解特性研究. 中国地质大学. [Zhang S. 2009. A study on disintergration behavior of granite residual soil in Guangzhou.China University of Geosciences] [56] 赵澄林,吴崇筠. 1987. 油区岩相古地理. 北京: 石油工业出版社. [Zhao C L,Wu C J. 1987. Lithofacies Palaeogeography of Oilfields. Beijing: Petroleum Industry Press] [57] 赵澄林,朱筱敏. 2001. 沉积岩石学. 北京: 石油工业出版社. [Zhao C L,Zhu X M. 2001. Sedimentology. Beijing: Petroleum Industry Press] [58] 朱筱敏. 2008. 沉积岩石学. 北京: 石油工业出版社. [Zhu X M. 2008. Sedimentology. Beijing: Petroleum Industry Press] [59] Allen J R L. 1965. A review of the origin and characteristics of recent alluvial sediments.Sedimentology,5(2):89-191. [60] Brian J S,Stephen C P. 1987. Physical Geology: Study Guide. New York: Wiley. [61] Cant D J, Walker R G. 1978. Fluvial processes and facies sequence in the sandy braided South Saskatchewan River,Canda.Sedimentology,25(5):625-648. [62] Collinson J L. 1983. Modern and Ancient Fluvial Systems. Blackwell Scientific Publications. [63] David L. 1991. The Earth System:An Introduction to Earth Science.Wm. C. Brown Publishers. [64] Grzegorz J P,Zbigniew S, Piotr M. 2015. Application of OSL dating and 137 Cs measurements to reconstruct the history of water erosion:A case study of a Holocene colluvium in Swierklany,south Poland.Quaternary International,374:189-197. [65] Grzegorz J P,Zbigniew S,Piotr M. 2011. Some aspects of age assessment of Holocene loess colluvium:OSL and 137 Cs dating of sediment from Biata agricultural area,South Poland.Quaternary International,240(1-2):44-51. [66] Grzegorz J P,Zbigniew S,Piotr M. 2013. Influence of pedon history and washing nature on luminescence dating of Holocene colluvium on the example of research on the Polish loess areas.Quaternary International,296:61-67. [67] Jaremski J. 1994. Proposal for the method of stating the value of maximum swelling of the soil on the example of Opole marls eluvium. In:Geotechnics in the African environment. Rock Mechanics and Mining Sciences,2:545-554. [68] Neymark L A,Paces J B. 2013. Ion-probe U-Pb dating of authigenic and detrital opal from Neogene-Quaternary alluvium.Earth and Planetary Science Letters,361(1):98-109. [69] Matthias L,Jörg V. 2006. Colluvium:Definition,differentiation,and possible suitability for reconstructing Holocene climate data.Quaternary International,162-163:133-140. [70] Miall A D. 1978. Fluvial Sedimentology Memoir 5. Calgary: Canadian Society of Petroleum Geologists. [71] Miall A D. 1996. The Geology of Fluvial Deposits. Berlin: Springer. [72] Michal G,Helena H,Krzysztof S. 2014. Middle Pleistocene carbonate-cemented colluvium in southern Poland:Its depositional processes,diagenesis and regional palaeoenvironmental significance.Sedimentary Geology,306,:24-35. [73] Piotr G,Andrij J,Marek K, Anna B, Natalia C, Leszek S, Wiaczeslaw A, Bogan R. 2015. Stratigraphy of alluvia and phases of the Holocene floods in the valleys of the Eastern Carpathians foreland.Quaternary International:1-12. doi:10.1016/j.quaint.2015.11.088. [74] Reading H G. 1985. 沉积环境和相. 北京: 科学出版社. [Reading H G. 1985. Depositional Environment and Facies. Beijing: Scince Press] [75] Reineck H E,Singh I B. 1978. 陆源碎屑沉积环境. 北京: 石油工业出版社. [Reineck,Singh I B. 1979. Terrigenous Clastic Depositional Environment. Beijing: Petroleum Industry Press] [76] Richard A D. 1992. Depositional System: An Introduction to Sedimentology and Stratigraphy(Second edition). New Jersey: Prentic Hall, Engewood Cliffs. [77] Ronald C C,Madhav K M,Lewis A O, Shannon A M, Michele G. 2015. Late Quaternary chronostratigraphic framework of terraces and alluvium along the lower Ohio River, southwestern Indiana and western Kentucky, USA. Quaternary Science Reviews,110: 72-91. [78] Walker. 1979. 沉积相模式. 地质部情报研究所. [Walker. 1979. Depositional Models. Geological Information Institute] [79] Willy A L. 2007. Landslide initiation in saprolite and colluvium in southern Brazil: Field and laboratory observations.Geomorphology,87(3):104-119. [80] Zolnikov I D,Deev E V,Nazarov D V. 2015. Comparative analysis of megaflood deposits and alluvium of the Chuya and Katun’ river valleys(Gorny Altai).Russian Geology and Geophysics,56(8):1162-1172.
