深水碳酸盐沉积研究进展

摘要/Abstract

摘要： 深水碳酸盐沉积包括深水重力流作用形成的异地沉积和非重力流沉积, 在非重力流沉积中又有深水牵引流(等深流、内波、内潮汐等) 沉积和静态原地碳酸盐沉积。深水碳酸盐沉积与重力流及等深流活动有关, 也受控于表层水碳酸盐产率、陆源物质的稀释作用及深水对碳酸盐的溶解作用。大量研究表明, 深水碳酸盐沉积对海平面升降与气候变化响应明显,无论是重力流或非重力流沉积均有体现, 通过深水碳酸盐沉积研究可以提取地质历史时期环境变化的信息, 同时,某些深水碳酸盐沉积岩中蕴藏着丰富的石油、天然气和其他沉积矿产。由此开展此项研究具有重要的理论和实际意义。

关键词: 深水碳酸盐, 海平面升降, 气候变化, 沉积响应

Abstract: Deep water carbonate sediments include allochthonous carbonate sediments released from shallow water by gravity flow and carbonate contourite and static autochthonous deep sea carbonate sediments. Deep water carbonate sediments were controlled by gravity flow, contoured flow and also controlled by carbonate productivity of surface water, dilution of siliciclastic from the land, and carbonate corrosion under deep sea. Most researches indicate that deep water carbonate sediments perfectly response to sea level variations and climatic changes no matter whether gravity flow or no gravity sediments. The information about environmental evolution can be obtained through studying on deep water carbonate sediments. Meanwhile, there are rich oil, natural gas and other sedimentary mineral resources in deep water carbon ate rocks. So, there are important theoretical and applied significances.

Key words: deep water carbonate sediment, sea level variation, climatic change, sedimentary response

中图分类号:

P512.2

朱井泉, 江茂生, 李学杰. 深水碳酸盐沉积研究进展[J]. 古地理学报, 2001, 3(4): 61-68.

Jiang Maosheng, Zhu Jingquan, Li Xuejie. NEW PROGRESS IN RESEARCH ON DEEP WATER CARBONATE SEDIMENTATION[J]. JOPC, 2001, 3(4): 61-68.

/ / 推荐 / 导出引用

链接本文: http://www.gdlxb.cn/CN/Y2001/V3/I4/61

参考文献

[1] 郭成贤. 我国深水异地沉积研究三十年. 古地理学报,2000,2(1):1~10
[2] Cook HE, EnosP著:冯增昭等译. 深水碳酸盐环境. 北京: 地质出版社, 1987.1~259
[3] 高振中,段太忠. 湘西黔东寒武纪深水碳酸盐重力流沉积. 沉积学报,1985,3(3):7~22
[4] 梅志超,李文厚. 陕西富平中上奥陶统深水碳酸盐重力流沉积模式.沉积学报,1986,4(1):34~42
[5] 高振中,段太忠. 滇西北泥盆纪海槽中的陆源碎屑海底扇及坡脚碳酸盐异地沉积. 石油与天然气地质,1986,7(4):308~323
[6] 王一刚. 黔南桂西早三叠世大陆斜坡碳酸盐重力流沉积. 沉积学报, 1986, 4(4): 91~100
[7] 刘宝, 张锦泉, 叶红专. 黔西南中三叠世陆棚一斜坡沉积特征. 沉积学报, 1987, 7(2): 1~15
[8] 金鹤生. 中三叠世滇黔桂深海盆的北侧被动陆缘.沉积学报, 1989,7(2):63~70
[9] 高振中,刘怀波. 十万大山盆地北缘早三叠世碳酸盐重力流及其地质意义. 石油与天然气地质,1983,4(1):55~65
[10] 晋慧娟,李育慈. 西秦岭早三叠世深水碳酸盐沉积演化模式.中国科学(B辑),1994, 24(8):890~896
[11] 高振中等. 深水牵引流沉积--内潮汐、内波和等深流沉积研究. 北京:科学出版社,1996. 1~112
[12] 段太忠,郭建华,高振中等. 华南古大陆边缘湘北九溪下奥陶统碳酸盐等深岩丘. 地质学报,1990,64(2):131~143
[13] Duan T, Gao Z, Zeng Y, et al.A fossil carbonate contourite drift on the Lower Ordovician palaeocontinental margin of the Middle Yangtze Terrane, Jiuxi, northern Hunan, Southern. China Sedimentary Geology, 1993, 82: 271~284
[14] 高振中,罗顺社,何幼斌等.鄂尔多斯地区西缘中奥陶世等深流沉积.沉积学报,1995,13(4):16~25
[15] 高振中,何幼斌,张兴阳等.塔中地区中奥陶世内波内潮汐沉积. 沉积学报,2000,18(3):400~407
[16] Shepard F P, Marshall N F, Mcloughlin P A, et al.Currents in submarine canyons and other seavalleys. AAPG Studies in Geology, 1979, 8:1~13
[17] Cacchione D A, Schawb W C, Noble M, et al.Internal tides and sediment movement on Horizon guyot, Mid-Pacific mountains. Geo Mar Lett,1988,8(1):21~28
[18] Gao Zhenzhong, Eriksson K A.Internal-tide deposits in an Ordovician submarine channel: Previously unrecognized facies? Geology, 1991,11(19):734~737
[19] 高振中, 何幼斌, 李建明等. 我国发现内潮汐沉积. 科学通报,1997,42(13):1418~1421
[20] 何幼斌, 高振中. 内潮汐、内波沉积的特征与鉴别. 科学通报,1998,43(9):903~908
[21] 张兴阳. 深水牵引流形成的床形单元组合.古地理学报,2000,2(2):28~26
[22] 李学杰, 段威武, 魏国彦等. 近2万年来南海北部与西部碳酸盐旋回及其古海洋学意义. 海洋地质与第四纪地质, 1997.16(3): 67~79
[23] Archer D E, Emerson S, Reimers C.Dissolution of calcite in deep sea sediments: Ph and 0₂ microelectrode results. Geochim Cosmochim Acta,1989,53:2831~2846
[24] Archer D E.An atlas of the distribution of calcium carbonate in sediments of the deep sea. Giobal Biogeochem Cycles, 1996, 10: 159~174
[25] Berger W H.Deep sea carbonates: Pleistocene dissolution cycles. J Foraminiferal Res, 1993,3: 187~195
[26] Pisias N G, Rea D K.Late Pleistocene paleoclimatology of the central equatorial Pacific: Sea surface response to the southeast trade winds. Paleoceanography, 1998,3:21~37
[27] Farrell J W, Prell W L.Climatic change and CaCO₃ preservation: An 800 000 years bathymetic reconstruction from the central equatorial Pacific Ocean. Paleoceanography,1989,4:447~466
[28] Farell J W, Prell W L.Pacific CaCO₃ preservation and δ¹⁸O since 4 Ma. Paleoceanography,1991,6:485~498
[29] Berelson W M, Hanond D E, McManus J, et al. Dissolution kinetics of calcium carbonate in equatorial Pacific sediments. Global Bilgeochem Cycles,1994,8:219~235
[30] Arrhenius C.Rate of production, dissolution, and accumulation of biogenic solids in the ocean Palaeogeos, Palaeoclimatol, Palaeoecol. 1988.67:119~146
[31] Archer D E.Equatorial Pacific calcite preservation cycles: Production or dissolution? Paleoceanography, 1991, 6:561~571
[32] Lyle M, Muray D W, Finney B P, et al.The record of Late Pleistocene biogenic sedimentation in the eastern tropical Pacific Ocean. Paleoceanogmaphy,1988,67:39~59
[33] Rea D K, Pisias N G, Newberry T.Late Pleistocene palaeoclimatology of the central equatorial Pacific: Flux patterns of biogenic sediments. Paleoceanogrphy,1991,6:227~244
[34] Berger W H.Pacific carbonate cycles revisited: Arguments for and against productivity control In: lshizaki K and Saito T, eds Centenary of Japanese Micropaleontology: Tokyo: Terra Scientific,1992 15~25
[35] Kutipers A, Duin E J.Th Boundary current-controlled turbidite deposition: A sedimentation model for the southern Nares abysal plain, western North Atlantic. Geo-Marine Letters, 1986,6:21~28
[36] Soh w, Tokuyama H, Fujoika K, et al. Morphology and development of a deep-sea meadering canyon (Boso Canyon) on an active plate margin, Sagami Trough. Japan Marine Geology,1990,91:227~241
[37] Anderson R F, Bacon M P, Brewer P G.Removal of ²³⁰Th and ²³¹Pa from the open ocean. Earth Planet Sci Lett ,1983,62:7~23
[38] Stephens M P, Kadko D C.Glacia-Holocene calcium carbonate dissolution at the central equatorial Pacific Seafloor. Paleoceanography,1997,12:797-804
[39] Bacon M P.Glacial to interglacial changes in carbonate and clay sedimentation in the Atlantic Ocean estimated from Th measurements Isot Geosci. 1984.2: 97~111
[40] Suman D 0, Bacon M P. Variations in Holocene sedimentation in North American Basin determined from ²³⁰Th measurements. Deep Sea Res,1989,36:869~878
[41] Taguchi K, Hlarada K, Tsunoeai S.Particulate removal of Th and Pa in the biologically productive northern North Pacific. Earh Planet Sci Lett ,1989,93:223~232
[42] Kumar N, Gwiazda R, Anderson R F, et al.²³¹Pa ²³⁰Th ratios in sediments as a proxy for past changes in Southern Ocean productivity. Nature,1993,362:45~48
[43] Berelson W M.Biogenic budgets of particle main, benthic remineralization and sediment accumulation in the equatorial Pacific. Dep Sea Res ,1997,9:25~37
[44] 汪品先. 西太平洋边缘海的冰期碳酸盐旋回. 海洋地质与第四纪地质,1998,18(I):1~11
[45] Stephens M P, Kadko D C, Smith C R,et al.Chlorophylla and phaeopigments as tracers of labile organic carbon at the central equatorial Pacific seafloor. Geochim Cosmochim Acta,1997,61:2231~2241
[46] Neftel A, Oeschger H, Stalielbach T et al. C0₂ record in the Byrd ice core 50000~5000 years BP. Nature,1988,331:609~611
[47] Keir R S, Michel R L.Interface dissolution control of the ¹⁴C profile in marine sediment. Geochim Cosmochim Acta,1993,57: 3562~3573
[48] Dromart G, Feny S and Atrps F. Allochthonous deep water carbonates and relative sea level changes: The Upper Jurassic-Lowemost Cretaceous of Southeast France. Spec Publs Int Ass Sediment,1993,18:295~305
[49] Haq B U.Deep sea response to eustatic change and significance of gas hydrates continental margin stratigraphy. Spec Publs lnt Ass Sediment,1993,18:93~106
[50] Miller R P, Heller P L.Depositional framework and controls on mixed carbonate-siliciclastic gravity flows: Pennsylvanian-Permian shelf to basin transect, South-Western Great Basin. USA Sedimentology, 1994,41(1):1~20
[51] Kola V, Macurda Jr D B. Sea level changes and timing of turbidity-current events in deep sea fans systems in: Wilgus C K, et al. , eds Sea level changes: An integrated approach. SEPM Spec Pubul ,1988,42:381~392
[52] Mitchum R M Jr. Seismic stratigraphic expression of submarine fan In: Berg 0 R, Woolverton D C, eds Seismic stratigraphy 2: An integrated approach to hydrocarbon exploration. Mem Am Assoc Petrl Geol, 1985, 39: 117~138
[53] Posamentier H W, Vail P R.Eustatic controls on clastic deposition 2-sequence and systems tact model in: Wilgus C K, et al. eds Sea level changes: An integrated approach. SEPM Spec Publ,1988,42: 125~154
[54] Shanmugan G, Moiola R J.Submarine fans: Characteristics, models, classification and reservoir potential. Earth Sci Rev, 1988, 24: 383~408
[55] Vail P R, Michum R M Jr. Thompson S Seismic stratigraphy and global changes of sea level In: Payon E D, ed. Seismic stratigraphy-Applications in hydrocarbon exploration. Mem Amer Ass Petrol ,1977,26:49~212
[56] Boardman M R, Neumann A C.Sources of periplalform carbonales: Northwest Providence Channel, 16 Bahamas. J Sediment Petrol,1984,54:1110~1123
[57] Droxler A w, Schlager w. Glacial versus interglacial sedimentation rates and turbidite frequency in the Bahamas. Geology, 1985, 13: 779~802
[58] Mullins H T.Comment of eustatic control of turbidites and winnowed turbidites. Geology,1983, 11:57~58
[59] Reymer J C, Schlager w, Droxler A W. Site 632: Pliocene-Pleistocene sedimentation cycles in a Bahamian Basin In: Austin J A, Schlager W, eds Proc ODP, Sci. Results 101 College Station Texas (Ocean Drilling Program).1988 213~220
[60] Schlager W, Ginsburg R N.Bahama carbonate platform-The deep and past. Mar Geol ,1981,44:1~24
[61] Cook H E, Taylor M E.Carbonate slope failures as indicators of sea-level lowerings. Bull Am Assoc Petrol Geol (Convention lssue), 1991,75(3):556
[62] Jacquin T, Amaud Vanneau A, Amaud H, Ravenne C, Vail P R.Systems tracts and depositional sequences in a carbonate setting: A study of continuous outcrops from platform to basin at the scale of seismic lines. Mar Petrol Geol, 1991, 8: 122~137
[63] Sang J F.Carbonate sequence stratigraphy In: Wilgus C K, et al., Hastings B S, Kendall C G St C, Posameter H W, Ross C A, Van C Wagoner J C, eds. Sea level changes: An integrated approach. SPEM Spec Publ, 1988,42:155~181
[64] Vail P R, Audemart F, Bowman S A, Eisner P N, Perez Cruz C.The stratigraphic signatures of tectonic, eustasy and sedimentology—An overview In: Einsele G, Ricken W, Seilacher A, eds Cycles and events in stratigraphy. Berlin: Spinger-Verlag,1991,617~-659
[65] 李粹中. 南海深水碳酸盐沉积作用. 沉积学报,1989,7(2):35~3
[66] 吴时国,涂霞,罗又郎. 南沙群岛海区晚第四纪深海碳酸盐沉积作用. 海洋地质与第四纪地质,1996,16(3):67~79
[67] Boer P l. Pelagic black shale-carbonate rhythms: Orbital forcing and oceanographic response. In: Einsele G, Ricken W, Seilacher A, eds. Cycles and events in stratigraphy Berlin: Springer Verlag,1991,63~78
[68] Fischer A G.Orbital cyclicity in Mesozoic strata. In: Einsele G, Ricken W, Seilacher A, eds. Cycles and events in stratigraphy Berlin: Springer Verlag,1991.48~62
[69] Diest-Huass l. Rhythmic carbonate content variations in Neogene sediments above the ocean lysocline. In: Einsele G, Ricken w, Seilacher A, eds. Cycles and events in stratigraphy Berlin: Springer-Verlag,1991.94~109
[70] Einsele G, Ricken W.Limestone-mari alteration-An overview. In: Einsele G, Ricken W, Seilacher A, eds. Cycles and events in stratigraphy Berin: Springer verag,1991.23~47
[71] Wiliams D F.Evidence for and against sea level changes from the stable isotopic record of the Cenozoic. In: Wilgus C K,et a. , eds. Sea level changes: An integrated approach. SEPM Spec Publ, 1988, 42:31~37

选择文件类型/文献管理软件名称

选择包含的内容