Acta Petrolei Sinica ›› 2025, Vol. 46 ›› Issue (10): 1970-1984.DOI: 10.7623/syxb202510011
• REVIEW • Previous Articles
Li Xiangdong1, Huan Yaqi2, Yang Min1, Zhang Linke3
Received:2024-05-07
Revised:2025-03-04
Published:2025-11-04
李向东1, 郇雅棋2, 杨敏1, 张林科3
通讯作者:
李向东,男,1973年2月生,2010年获长江大学博士学位,现为昆明理工大学国土资源工程学院副教授,主要从事沉积学研究与教学工作。
作者简介:李向东,男,1973年2月生,2010年获长江大学博士学位,现为昆明理工大学国土资源工程学院副教授,主要从事沉积学研究与教学工作。Email:lixiangdong614@163.com
基金资助:CLC Number:
Li Xiangdong, Huan Yaqi, Yang Min, Zhang Linke. Ponded turbidites in stratigraphic records[J]. Acta Petrolei Sinica, 2025, 46(10): 1970-1984.
李向东, 郇雅棋, 杨敏, 张林科. 地层记录中的阻塞浊流沉积[J]. 石油学报, 2025, 46(10): 1970-1984.
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| [1] PATACCI M, HAUGHTON P D W, MCCAFFREY W D.Flow behavior of ponded turbidity currents[J].Journal of Sedimentary Research, 2015, 85(8):885-902. [2] MUTTI E, BERNOULLI D, RICCI LUCCHI F, et al.Turbidites and turbidity currents from Alpine 'flysch’ to the exploration of continental margins[J].Sedimentology, 2009, 56(1):267-318. [3] SHANMUGAM G.50 years of the turbidite paradigm (1950s-1990s):deep-water processes and facies models―a critical perspective[J]. Marine and Petroleum Geology, 2000, 17(2):285-342. [4] HERSEY J B.Sediment ponding in the deep sea[J].GSA Bulletin, 1965, 76(11):1251-1260. [5] SKIPPER K.Antidune cross-stratification in a turbidite sequence, Cloridorme Formation, Gaspé, Quebec[J].Sedimentology, 1971, 17(1/2): 51-68. [6] WALKER R G.Deep-water sandstone facies and ancient submarine fans:models for exploration for stratigraphic traps[J].AAPG Bulletin, 1978, 62(6):932-966. [7] 庞雄, 陈长民, 朱明, 等.深水沉积研究前缘问题[J].地质论评, 2007, 53(1):36-43. PANG Xiong, CHEN Changmin, ZHU Ming, et al.Frontier of the deep-water deposition study [J].Geological Review, 2007, 53(1):36-43. [8] SHANMUGAM G, MOIOLA R J.Reinterpretation of depositional processes in a classic flysch sequence (Pennsylvanian Jackfork Group), Ouachita Mountains, Arkansas and Oklahoma[J].AAPG Bulletin, 1995, 79(5):672-695. [9] KNELLER B, BUCKEE C.The structure and fluid mechanics of turbidity currents:a review of some recent studies and their geological implications[J].Sedimentology, 2000, 47(S1):62-94. [10] CHEN Yuhang, YAO Genshun, WANG Xiaofeng, et al.Flow processes of the interaction between turbidity flows and bottom currents in sinuous unidirectionally migrating channels:an example from the Oligocene channels in the Rovuma Basin, offshore Mozambique[J].Sedimentary Geology, 2020, 404:105680. [11] CORNARD P H, PICKERING K T.Submarine topographic control on distribution of supercritical-flow deposits in lobe and related environments, Middle Eocene, Jaca Basin, Spanish Pyrenees[J].Journal of Sedimentary Research, 2020, 90(9):1222-1243. [12] SLOOTMAN A, VENTRA D, CARTIGNY M, et al.Supercritical-flow processes and depositional products:introduction to thematic issue[J].Sedimentology, 2021, 68(4):1289-1296. [13] MARINI M, PATACCI M, FELLETTI F, et al.Fill to spill stratigraphic evolution of a confined turbidite mini-basin succession, and its likely well bore expression:the Castagnola Fm, NW Italy[J].Marine and Petroleum Geology, 2016, 69:94-111. [14] CUNHA R S, TINTERRI R, MAGALHAES P M.Annot sandstone in the Pera Cava Basin:an example of an asymmetric facies distribution in a confined turbidite system (SE France)[J].Marine and Petroleum Geology, 2017, 87:60-79. [15] PATACCI M, MARINI M, FELLETTI F, et al.Origin of mud in turbidites and hybrid event beds:insight from ponded mudstone caps of the Castagnola turbidite system (north-west Italy)[J].Sedimentology, 2020, 67(5):2625-2644. [16] PATEL U S, GARDINER A, STOW D A V.Bed-scale vertical and lateral distribution of massive sandstone in a topographically confined basin (Pera Cava, SE France):implications for flow processes[J].Sedimentary Geology, 2021, 424:106001. [17] GORSLINE D S, EMERY K O.Turbidity-current deposits in San Pedro and Santa Monica basins off southern California[J].GSA Bulletin, 1959, 70(3):279-290. [18] RYAN W B F, WORKUM JR F, HERSEY J B.Sediments on the Tyrrhenian abyssal plain[J].GSA Bulletin, 1965, 76(11):1261-1282. [19] VAN ANDEL T H, KOMAR P D.Ponded sediments of the Mid-Atlantic ridge between 22° and 23° north latitude[J].GSA Bulletin, 1969, 80(7):1163-1190. [20] HISCOTT R N, PICKERING K T.Reflected turbidity currents on an Ordovician basin floor, Canadian Appalachians[J].Nature, 1984, 311(5982):143-145. [21] PICKERING K T, HISCOTT R N.Contained (reflected)turbidity currents from the Middle Ordovician Cloridorme Formation, Quebec, Canada:an alternative to the antidune hypothesis[J].Sedimentology, 1985, 32(3):373-394. [22] RICCI LUCCHI F, VALMORI E.Basin-wide turbidites in a Miocene, over-supplied deep-sea plain:a geometrical analysis[J].Sedimentology, 1980, 27(3):241-270. [23] TINTERRI R, PIAZZA A.Turbidites facies response to the morphological confinement of a foredeep (Cervarola Sandstones Formation, Miocene, northern Apennines, Italy)[J].Sedimentology, 2019, 66(2):636-674. [24] PIAZZA A, TINTERRI R, ARTONI A.The role of orogen-transversal tectonic structures on the "syn" and "post" depositional evolution of a foredeep succession:the case of the Cervarola Sandstones Formation, Miocene, northern Apennines, Italy[J].Tectonophysics, 2020, 778:228367. [25] EDWARDS D A, LEEDER M R, BEST J L, et al.On experimental reflected density currents and the interpretation of certain turbidites[J].Sedimentology, 1994, 41(3):437-461. [26] SEQUEIROS O E, SPINEWINE B, GARCIA M H, et al.Experiments on wedge-shaped deep sea sedimentary deposits in minibasins and/or on channel levees emplaced by turbidity currents.Part Ⅰ:documentation of the flow[J].Journal of Sedimentary Research, 2009, 79(8):593-607. [27] THEILER Q, FRANCA M J.Contained density currents with high volume of release[J].Sedimentology, 2016, 63(6):1820-1842. [28] SIWEK P, WAS ' KOWSKA A, WENDORFF M.Mud-rich low-density turbidites in structurally-controlled intraslope mini-basin:the influence of flow containment on depositional processes and sedimentation patterns (Szczawa, Oligocene, Polish Outer Carpathians)[J].Sedimentology, 2023, 70(6):1741-1784. [29] TINTERRI R, MAGALHAES P M, TAGLIAFERRI A, et al.Convolute laminations and load structures in turbidites as indicators of flow reflections and decelerations against bounding slopes.Examples from the Marnoso-arenacea Formation (northern Italy)and Annot sandstones (south eastern France)[J].Sedimentary Geology, 2016, 344:382-407. [30] 李向东, 陈洪达, 陈海燕, 等.鄂尔多斯盆地西缘上奥陶统拉什仲组包卷层理成因机制探讨[J].古地理学报, 2022, 24(6):1130-1148. LI Xiangdong, CHEN Hongda, CHEN Haiyan, et al.Genesis mechanism analysis of convolute laminations of the Upper Ordovician Lashenzhong Formation in western margin of Ordos Basin[J].Journal of Palaeogeography, 2022, 24(6):1130-1148. [31] GLADSTONE C, MCCLELLAND H L O, WOODCOCK N H, et al.The formation of convolute lamination in mud-rich turbidites[J].Sedimentology, 2018, 65(5):1800-1825. [32] TONIOLO H, LAMB M, PARKER G.Depositional turbidity currents in diapiric minibasins on the continental slope:formulation and theory [J].Journal of Sedimentary Research, 2006, 76(5):783-797. [33] KHAN S M, IMRAN J.Numerical investigation of turbidity currents flowing through minibasins on the continental slope[J].Journal of Sedimentary Research, 2008, 78(4):245-257. [34] ATHMER W, GROENENBERG R M, LUTHI S M, et al.Relay ramps as pathways for turbidity currents:a study combining analogue sandbox experiments and numerical flow simulations[J].Sedimentology, 2010, 57(3):806-823. [35] MAGALHAES P M, TINTERRI R.Stratigraphy and depositional setting of slurry and contained (reflected)beds in the Marnoso-arenacea Formation (Langhian-Serravallian)northern Apennines, Italy[J].Sedimentology, 2010, 57(7):1685-1720. [36] TÖKÉS L, PATACCI M.Quantifying tabularity of turbidite beds and its relationship to the inferred degree of basin confinement[J].Marine and Petroleum Geology, 2018, 97:659-671. [37] LIU Qun, KNELLER B, FALLGATTER C, et al.Tabularity of individual turbidite beds controlled by flow efficiency and degree of confinement[J].Sedimentology, 2018, 65(7):2368-2387. [38] TINTERRI R, MAGALHAES P M.Synsedimentary structural control on foredeep turbidites:an example from Miocene Marnoso-arenacea Formation, northern Apennines, Italy[J].Marine and Petroleum Geology, 2011, 28(3):629-657. [39] TINTERRI R, TAGLIAFERRI A.The syntectonic evolution of foredeep turbidites related to basin segmentation:facies response to the increase in tectonic confinement (Marnoso-arenacea Formation, Miocene, northern Apennines, Italy)[J].Marine and Petroleum Geology, 2015, 67:81-110. [40] MCCAFFREY W, KNELLER B.Process controls on the development of stratigraphic trap potential on the margins of confined turbidite systems and aids to reservoir evaluation[J].AAPG Bulletin, 2001, 85(6):971-988. [41] DORRELL R M, PATACCI M, MCCAFFREY W D.Inflation of ponded, particulate laden density currents[J].Journal of Sedimentary Research, 2018, 88(11):1276-1282. [42] MARINI M, FELLETTI F, MILLI S, et al.The thick-bedded tail of turbidite thickness distribution as a proxy for flow confinement:examples from tertiary basins of central and northern Apennines (Italy)[J].Sedimentary Geology, 2016, 341:96-118. [43] PANTOPOULOS G, KNELLER B C, MCARTHUR A D, et al.Turbidite bed thickness statistics of architectural elements in a deep-marine confined mini-basin setting:examples from the Grès d'Annot Formation, SE France[J].Marine and Petroleum Geology, 2018, 95:16-29. [44] ETIENNE S, MULDER T, RAZIN P, et al.Proximal to distal turbiditic sheet-sand heterogeneities:characteristics of associated internal channels.Examples from the Trois Evêchés area, Eocene-Oligocene Annot sandstones (Grès d'Annot), SE France[J].Marine and Petroleum Geology, 2013, 41:117-133. [45] SALLES L, FORD M, JOSEPH P.Characteristics of axially-sourced turbidite sedimentation on an active wedge-top basin (Annot sandstone , SE France)[J].Marine and Petroleum Geology, 2014, 56:305-323. [46] MUTTI E.Distinctive thin-bedded turbidite facies and related depositional environments in the Eocene Hecho Group (South-central Pyrenees , Spain)[J].Sedimentology, 1977, 24(1):107-131. [47] BAYLISS N J, PICKERING K T.Deep-marine structurally confined channelised sandy fans:Middle Eocene Morillo System, Ainsa Basin, Spanish Pyrenees[J].Earth-Science Reviews, 2015, 144:82-106. [48] MARINI M, MILLI S, RAVNÅS R, et al.A comparative study of confined vs.semi-confined turbidite lobes from the Lower Messinian Laga Basin (Central Apennines, Italy):implications for assessment of reservoir architecture[J].Marine and Petroleum Geology, 2015, 63:142-165. [49] FLINT S S, HODGSON D M, SPRAGUE A R, et al.Depositional architecture and sequence stratigraphy of the Karoo Basin floor to shelf edge succession, Laingsburg depocentre, South Africa[J].Marine and Petroleum Geology, 2011, 28(3):658-674. [50] GRECULA M, FLINT S, POTTS G, et al.Partial ponding of turbidite systems in a basin with subtle growth-fold topography:Laingsburg-Karoo, south Africa[J].Journal of Sedimentary Research, 2003, 73(4):603-620. [51] JI Shaocheng, CHEN Tiantian, LI Le, et al.Characterization of carbonate veins in graywacke layers from the Humber zone (Quebec, Canada)and implications for strength recovery of damaged rocks by mineral precipitation[J].Tectonophysics, 2023, 868:230084. [52] KNELLER B, MCCAFFREY W.Depositional effects of flow nonuniformity and stratification within turbidity currents approaching a bounding slope:deflection, reflection, and facies variation[J].Journal of Sedimentary Research, 1999, 69(5):980-991. [53] 李向东.浅议沉积学中的流体问题[J].世界地质, 2020, 39(1):45-55. LI Xiangdong.An overview of hydromechanics in sedimentology[J].Global Geology, 2020, 39(1):45-55. [54] LAMB M P, HICKSON T, MARR J G, et al.Surging versus continuous turbidity currents:flow dynamics and deposits in an experimental intraslope minibasin[J].Journal of Sedimentary Research, 2004, 74(1):148-155. [55] ITO M.Downfan transformation from turbidity currents to debris flows at a channel-to-lobe transitional zone:the Lower Pleistocene Otadai Formation, Boso Peninsula, Japan[J].Journal of Sedimentary Research, 2008, 78(10):668-682. [56] KNELLER B C, BRANNEY M J.Sustained high-density turbidity currents and the deposition of thick massive sands[J].Sedimentology, 1995, 42(4):607-616. [57] MUCK M T, UNDERWOOD M B.Upslope flow of turbidity currents:a comparison among field observations, theory, and laboratory models[J].Geology, 1990, 18(1):54-57. [58] PANTIN H M, LEEDER M R.Reverse flow in turbidity currents:the role of internal solitons[J].Sedimentology, 1987, 34(6): 1143-1155. [59] HISCOTT R N, AKSU A E, FLOOD R D, et al.Widespread overspill from a saline density-current channel and its interaction with topography on the south-west Black Sea shelf[J].Sedimentology, 2013, 60(7):1639-1667. [60] DODD T J H, MCCARTHY D J, RICHARDS P C.A depositional model for deep-lacustrine, partially confined, turbidite fans:Early Cretaceous, North Falkland Basin[J].Sedimentology, 2019, 66(1):53-80. [61] LOWE D R.Sediment gravity flows:Ⅱ.Depositional models with special reference to the deposits of high-density turbidity currents[J].Journal of Sedimentary Research, 1982, 52(1):279-297. [62] SOHN Y K.On traction-carpet sedimentation[J].Journal of Sedimentary Research, 1997, 67(3):502-509. [63] LIU Qun, KNELLER B, FALLGATTER C, et al.Quantitative comparisons of depositional architectures of unconfined and confined turbidite sheet systems[J].Sedimentary Geology, 2018, 376:72-89. [64] HAUGHTON P D W.Deposits of deflected and ponded turbidity currents, Sorbas Basin, Southeast Spain[J].Journal of Sedimentary Research, 1994, 64(2a):233-246. [65] FONNESU M, PATACCI M, HAUGHTON P D W, et al.Hybrid event beds generated by local substrate delamination on a confined-basin floor[J].Journal of Sedimentary Research, 2016, 86(8):929-943. [66] FELLETTI F.Complex bedding geometries and facies associations of the turbiditic fill of a confined basin in a transpressive setting (Castagnola Fm., Tertiary Piedmont Basin, NW Italy)[J].Sedimentology, 2002, 49(4):645-667. [67] CAMPBELL C V.Lamina, laminaset, bed and bedset[J].Sedimentology, 1967, 8(1):7-26. [68] HAUGHTON P D W.Evolving turbidite systems on a deforming basin floor, Tabernas, SE Spain[J].Sedimentology, 2000, 47(3):497-518. [69] REMACHA E, FERNNDEZ L P, MAESTRO E.The transition between sheet-like lobe and basin-plain turbidites in the Hecho Basin (south-central Pyrenees, Spain)[J].Journal of Sedimentary Research, 2005, 75(5):798-819. [70] SINCLAIR H D.Delta-fed turbidites infilling topographically complex basins:a new depositional model for the Annot sandstones, SE France[J].Journal of Sedimentary Research, 2000, 70(3):504-519. [71] FONNESU M, FELLETTI F, HAUGHTON P D W, et al.Hybrid event bed character and distribution linked to turbidite system sub-environments:the north Apennine Gottero Sandstone (north-west Italy)[J].Sedimentology, 2018, 65(1):151-190. [72] CAJA M A, MARFIL R, GARCIA D, et al.Provenance of siliciclastic and hybrid turbiditic arenites of the Eocene Hecho Group, Spanish Pyrenees:implications for the tectonic evolution of a foreland basin[J].Basin Research, 2010, 22(2):157-180. [73] NINGTHOUJAM J, WEARMOUTH C, ARNOTT R W C.Stratal characteristic and depositional origin of two-part (mud-poor overlain by mud-rich)and associated deep-water strata:components in a lateral depositional continuum related to particle settling in negligibly sheared mud -rich suspensions[J].Journal of Sedimentary Research, 2022, 92(6):503-529. [74] POYATOS-MORÉ M, JONES G D, BRUNT R L, et al.Clinoform architecture and along-strike facies variability through an exhumed erosional to accretionary basin margin transition[J].Basin Research, 2019, 31(5):920-947. [75] TINTERRI R, LAPORTA M, OGATA K.Asymmetrical cross-current turbidite facies tract in a structurally-confined mini-basin (Priabonian-Rupelian, Ranzano sandstone, northern Apennines, Italy)[J].Sedimentary Geology, 2017, 352:63-87. [76] WHITMORE J H, STROM H.Sand injectites at the base of the Coconino sandstone, Grand Canyon, Arizona (USA)[J].Sedimentary Geology, 2010, 230(1/2):46-59. [77] MAZUMDER R, VAN LOON A J, MALVIYA V P, et al.Soft-sediment deformation structures in the Mio-Pliocene Misaki Formation within alternating deep-sea clays and volcanic ashes (Miura Peninsula, Japan)[J].Sedimentary Geology, 2016, 344:323-335. [78] OGIWARA H, ITO M.Origin and internal organization of widespread composite soft-sediment deformation units in a deep-water forearc basin:the Lower Pleistocene Kazusa Group on the Boso Peninsula, Japan[J].Sedimentary Geology, 2011, 237(3/4):209-221. [79] 李向东, 何幼斌, 张铭记, 等.宁夏中奥陶统香山群徐家圈组内波、内潮汐沉积类型[J].地球科学进展, 2011, 26(9):1006-1014. LI Xiangdong, HE Youbin, ZHANG Mingji, et al.Sedimentary types of internal-wave and internal-tide deposits of Middle Ordovician, Xujiajuan Formation, Xiangshan Group, Ningxia Autonomous region, China[J].Advances in Earth Science, 2011, 26(9):1006-1014. [80] 李向东, 魏泽昳, 陈洪达.鄂尔多斯盆地西缘上奥陶统拉什仲组内波和内潮汐沉积成因分析[J].地质学报, 2023, 97(4):1278-1294. LI Xiangdong, WEI Zeyi, CHEN Hongda.Genetic analysis of internal-wave and internal-tide deposits in the Upper Ordovician Lashenzhong Formation, western Ordos Basin[J].Acta Geologica Sinica, 2023, 97(4):1278-1294. [81] 李向东, 陈海燕.深水环境下古水流方向分析和阻塞浊流沉积的识别——以鄂尔多斯盆地桌子山地区上奥陶统拉什仲组为例[J].石油学报, 2020, 41(11):1348-1365. LI Xiangdong, CHEN Haiyan.Analysis of paleocurrent direction and identification of ponded turbidity current deposits in deep water environment:a case study of the Upper Ordovician Lashenzhong Formation in Zhuozishan area, Ordos Basin[J].Acta Petrolei Sinica, 2020, 41(11):1348-1365. [82] 李向东, 魏泽昳, 陈海燕.深水阻塞盆地陆源碎屑岩地球化学特征分析——以鄂尔多斯盆地桌子山地区上奥陶统拉什仲组为例[J].中国矿业大学学报, 2024, 53(1):158-175. LI Xiangdong, WEI Zeyi, CHEN Haiyan.Geochemical characteristics analyses of terrigenous clastic rocks in deep-water ponded basin:a case study from Upper Ordovician Lashenzhong Formation in Zhuozishan area, Ordos Basin[J].Journal of China University of Mining & Technology, 2024, 53(1):158-175. [83] REMACHA E, FERNNDEZ L P.High-resolution correlation patterns in the turbidite systems of the Hecho Group (south-central Pyrenees, Spain)[J].Marine and Petroleum Geology, 2003, 20(6/8):711-726. [84] MANZI V, LUGLI S, RICCI LUCCHI F, et al.Deep-water clastic evaporites deposition in the Messinian Adriatic foredeep (northern Apennines, Italy):did the Mediterranean ever dry out?[J].Sedimentology, 2005, 52(4):875-902. [85] PRATHER B E, BOOTH J R, STEFFENS G S, et al.Classification, lithologic calibration, and stratigraphic succession of seismic facies of intraslope basins, deep-water Gulf of Mexico[J].AAPG Bulletin, 1998, 82(5A):701-728. [86] COUNTS J W, AMOS K J.Sedimentology, depositional environments and significance of an Ediacaran salt-withdrawal minibasin, Billy Springs Formation, Flinders Ranges, South Australia[J].Sedimentology, 2016, 63(5):1084-1123. [87] VALLE G D, GAMBERI F, TRINCARDI F, et al.Contrasting slope channel styles on a prograding mud-prone margin[J].Marine and Petroleum Geology, 2013, 41:72-82. [88] VARONA G M, FLEMINGS P B, PORTNOV A.Hydrate-bearing sands in the Terrebonne Basin record the transition from ponded deposition to bypass in the deep-water Gulf of Mexico[J].Marine and Petroleum Geology, 2023, 151:106172. |
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