Research Progress of Isolated Carbonate Platform
DOI:
https://doi.org/10.62051/ijnres.v5n3.06Keywords:
Isolated Carbonate Platform; Sedimentary Facies Model; Structural Evolution; Digital Geology; Research Methods.Abstract
Isolated carbonate platforms represent a distinct category within the morphological classification of carbonate platforms. Investigating their evolutionary processes encompassing formation, development, and demise holds significant implications for reconstructing basin tectonic evolution, restoring paleogeography, paleo-oceanographic conditions, and paleoclimate, exploring organism-environment co-evolution, deciphering celestial orbital parameter variations, and guiding hydrocarbon source rock evaluation and reservoir development. This study systematically reviews the definition and classification of isolated platforms, establishing an idealized sedimentary facies model based on Wilson's standard facies zones and modern analogs from the Great Bahama Bank. Special emphasis is placed on elucidating controlling factors and methodological approaches governing platform evolution and termination, accompanied by critical assessments of their research significance and practical applications. Notably, isolated carbonate platform research has evolved from traditional qualitative field outcrop analyses to modern multi-method quantitative-semi-quantitative approaches. The emergence of 2D/3D digital geological technologies and numerical simulation models enables three-dimensional visualization of stratigraphic frameworks and facies distribution, facilitating precise geological investigations. Future research should integrate tectonic processes, eustatic fluctuations, and paleoclimatic contexts while prioritizing carbonate producers' response to environmental fluctuations during platform evolution.
References
[1]Ding Zhongli. 2006. Milankovitch 's Glacial Cycle Theory: Challenges and Opportunities [J]. Quaternary Studies, 26 (5): 710-717.
[2]Gu, Ma, Ji, 2009.Types, characteristics and main controlling factors of carbonate platform [J]. Paleogeography, 11 (1): 21-27.
[3]Lu Gang, Liu Chao, Zhang Xi, Zhou Fusheng, Huang Xianglin, Du Yuansheng.Late Paleozoic sedimentary characteristics and evolution of Tian 'e isolated carbonate platform [J]. Geological review, pending publication.
[4]Shen Shi Guangyu, Liu Yuzhi. 2006. Advances in Milankovitch 's Theory of Earth Climate Change [J]. Advances in Earth Science, 21 (3): 278-285.
[5]Wang Xinqiang, Shi Xiaoying. 2008. Sedimentary characteristics and evolution stages of Late Paleozoic Leye isolated carbonate platform in northwestern Guangxi [J]. Paleogeography, 10 (4): 329-338.
[6]Yang Huaiyu, Chen Shiyue, Hao Xiaoliang, Guo Hua, Li Cong.2010.Sedimentary characteristics and evolution stages of Late Paleozoic Longlin isolated platform in Nanpanjiang Depression [J]. Geology of China, 37 (6): 1638-1645.
[7]Zhang ShihongAdams E W, Schroder S, Grotzinger J P, McCormick D S. 2004. Digital reconstruction and stratigraphic evolution of a microbial-dominated, isolated carbonate platform (terminal Proterozoic, Nama Group, Namibia) [J]. Journal of Sedimentary Research, 74(4): 479-497.
[8]Amour F, Mutti M, Christ N, Immenhauser A, Benson G S, Agar S M, Tomas S, Kabiri L. 2013. Outcrop analog for an oolitic carbonate ramp reservoir: A scale-dependent geologic modeling approach based on stratigraphic hierarchy[J]. AAPG Bulletin, 97(5): 845-871.
[9]Azmy K, Poty E, Brand U. 2009. High-resolution isotope stratigraphy of the Devonian–Carboniferous boundary in the Namur–Dinant Basin, Belgium[J]. Sedimentary Geology, 216(3): 117-124.
[10]Babek O, Prikryl T, Hladil J. 2007. Progressive drowning of carbonate platform in the Moravo-Silesian Basin (Czech Republic) before the Frasnian/Famennian event: facies, compositional variations and gamma-ray spectrometry[J]. Facies, 53(2): 293-316.
[11]Barnett A, Burgess P, Wright V. 2002. Icehouse world sea‐level behaviour and resulting stratal patterns in late Visean (Mississippian) carbonate platforms: integration of numerical forward modelling and outcrop studies[J]. Basin Research, 14(3): 417-438.
[12]Bassi D. 2005. Larger foraminiferal and coralline algal facies in an Upper Eocene storm-influenced, shallow-water carbonate platform (Colli Berici, north-eastern Italy) [J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 226(1): 17-35.
[13]Bechstädt T, Schledding T, Selg M. 1988. Rise and fall of an isolated, unstable carbonate platform: the Cambrian of Southwestern Sardinia[J]. Geologische Rundschau, 77(2): 389-416.
[14]Bergman K L, Westphal H, Janson X, Poiriez A, Eberli G P. 2010. Controlling parameters on facies geometries of the Bahamas, an isolated carbonate platform environment. In: Carbonate Depositional Systems: Assessing Dimensions and Controlling Parameterss(Ed. by Westphal H, Riegl B & Eberli G P), Springer, 5-80.
[15]Betzler C, Fürstenau J, Lüdmann T, Hübscher C, Lindhorst S, Paul A, Reijmer J J, Droxler A W. 2012. Sea‐level and ocean‐current control on carbonate‐platform growth, Maldives, Indian Ocean[J]. Basin Research, 25, 172-196.
[16]Betzler C, Hübscher C, Lindhorst S, Reijmer J J, Römer M, Droxler A W, Fürstenau J, Lüdmann T. 2009. Monsoon-induced partial carbonate platform drowning (Maldives, Indian Ocean) [J]. Geology, 37(10): 867-870.
[17]Boni M & Selg M. 1985. The Lower Cambrian of SW-Sardinia: from a clastic tidal shelf to an isolated carbonate platform[J]. Facies, 12(1): 113-139.
[18]Bosence D. 2005. A genetic classification of carbonate platforms based on their basinal and tectonic settings in the Cenozoic [J]. Sedimentary Geology, 175, 49-72.
[19]Bosence D, Cross N, Hardy S. 1998a. Architecture and depositional sequences of Tertiary fault-block carbonate platforms; an analysis from outcrop (Miocene, Gulf of Suez) and computer modelling[J]. Marine and Petroleum Geology, 15(3): 203-221.
[20]Brun, J P & Fort X. 2011. Salt tectonics at passive margins: Geology versus models[J]. Marine and Petroleum Geology, 28(6): 1123-1145.
[21]Burchette T P & Wright V P. 1992. Carbonate ramp depositional systems[J]. Sedimentary Geology, 79(1-4): 3-57.
[22]Burgess P M. 2001. Modeling carbonate sequence development without relative sea-level oscillations[J]. Geology, 29(12): 1127-1130.
[23]Burgess P M. 2011. CarboCAT: A cellular automata model of heterogeneous carbonate strata[J]. Computers & Geosciences, 53: 129-140.
[24]Burgess P M, Wright V P. 2003. Numerical forward modeling of carbonate platform dynamics: An evaluation of complexity and completeness in carbonate strata[J]. Journal of Sedimentary Research, 73(5): 637-652.
[25]Carpentier C, Lathuiliere B, Ferry S. 2010. Sequential and climatic framework of the growth and demise of a carbonate platform: implications for the peritidal cycles (Late Jurassic, North-eastern France) [J]. Sedimentology, 57, 985-1020.
[26]Chen D Z, Tucker M E, Jiang M S, Zhu J Q. 2001. Long-distance correlation between tectonic-controlled, isolated carbonate platforms by cyclostratigraphy and sequence stratigraphy in the Devonian of South China[J]. Sedimentology, 48(1): 57-78.
[27]Da Silva A C & Boulvain F. 2006. Upper Devonian carbonate platform correlations and sea level variations recorded in magnetic susceptibility[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 240(3): 373-388.
[28]Eberli G P. 1991. Growth and demise of isolated carbonate platforms: Bahamian controversies[J]. Controversies in Modern Geology, 231-248.
[29]Egenhoff S O, Peterhänsel A, Bechstädt T, Zühlke R, Grötsch J. 1999. Facies architecture of an isolated carbonate platform: tracing the cycles of the Latemar (Middle Triassic, northern Italy) [J]. Sedimentology, 46(5): 893-912.
[30]Ehrenberg S N, McArthur J M, Thirlwall M F. 2006. Growth, demise, and dolomitization of Miocene carbonate platforms on the Marion Plateau, offshore NE Australia[J]. Journal of Sedimentary Research, 76(1-2): 91-116.
[31]Erlich R N, Longo A P, Hyare S. 1993. Response of platform margins to drowning; evidence of environmental collapse. In: Carbonate sequence stratigraphy recent developments and applications(Ed. by Loucks R G & Sarg J F). AAPG Bulletin 57, 241-266.
[32]Falivene O, Arbués P, Howell J, Muñoz J, Fernández O, Marzo M. 2006. Hierarchical geocellular facies modelling of a turbidite reservoir analogue from the Eocene of the Ainsa Basin, NE Spain[J]. Marine and Petroleum Geology, 23(6): 679-701.
[33]Fernandez-Mendiola P A, Garcia-Mondejar J. 1997. Isolated carbonate platform of Caniego, Spain: A test of the latest Albian worldwide sea-level changes[J]. Geological Society of America Bulletin, 109(2): 176-194.
[34]Flèugel E & Munnecke A. 2010. Microfacies of carbonate rocks: analysis, interpretation and application[M].New York: Springer-Verlag Berlin Heidelberg, 26-725.
[35]Föllmi K B, Weissert H, Bisping M, Funk H. 1994. Phosphogenesis, carbon-isotope stratigraphy, and carbonate-platform evolution along the Lower Cretaceous northern Tethyan margin[J]. Geological Society of America Bulletin, 106(6): 729-746.
[36]Fornos J J & Ahr W M.1997. Temperate carbonates on a modern, low-energy, isolated ramp: the Balearic platform, Spain[J]. Journal of Sedimentary Research, 67(2): 364-373.
[37]Fornos J J & Ahr W M. 2006. Present-day temperate carbonate sedimentation on the Balearic Platform, western Mediterranean: compositional and textural variation along a low-energy isolated ramp[J]. Geological Society, London, Special Publications, 255(1): 71-84.
[38]Fugagnoli A. 2004. Trophic regimes of benthic foraminiferal assemblages in Lower Jurassic shallow water carbonates from northeastern Italy (Calcari Grigi, Trento Platform, Venetian Prealps) [J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 205(1): 111-130.
[39]Fyhn M B W, Boldreel L O, Nielsen L H. 2009. Tectonic and climatic control on growth and demise of the Phanh Rang Carbonate Platform offshore south Vietnam[J]. Basin Research, 21(2): 225-251.
[40]Fyhn M B, Boldreel L O, Nielsen L H, Giang T C, Nga L H, Hong N, Nguyen N D, Abatzis I. 2013. Carbonate platform growth and demise offshore Central Vietnam: Effects of Early Miocene transgression and subsequent onshore uplift[J]. Journal of Asian Earth Sciences, http://dx.doi.org/10.1016/j.jseaes.2013.02.023
[41]García-Mondéjar J. 1990. The Aptian–Albian carbonate episode of the Basco-Cantabrian Basin (N-Spain): general characteristics, controls, and evolution. In: Carbonate Platforms (Ed. by Tucker M E, Wilson J L, Crevello P D, Sarg J F, Read J F), IAS Special Publication, 9, 291-323.
[42]Gatt P & Gluyas J. 2012. Climatic controls on facies in Palaeogene Mediterranean subtropical carbonate platforms[J]. Petroleum Geoscience, 18(3): 355-367.
[43]George A D, Chow N, Trinajstic K M. 2009. Syndepositional fault control on lower Frasnian platform evolution, Lennard Shelf, Canning Basin, Australia[J]. Geology, 37(4): 331-334.
[44]Gischler E. 1994. Sedimentation on three Caribbean atolls: Glovers reef, Lighthouse reef and Turneffe islands, Belize[J]. Facies, 31(1): 243-254.
[45]Gischler E, Hauser I, Heinrich K, Scheitel U. 2003. Characterization of depositional environments in isolated carbonate platforms based on benthic foraminifera, Belize, Central America[J]. Palaios, 18(3): 236-255.
[46]Gischler E & Lomando A J. 1999. Recent sedimentary facies of isolated carbonate platforms, Belize-Yucatan System, Central America[J]. Journal of Sedimentary Research, 69(3): 747-763.
[47]Gischler E, Lomando A J, Hudson J H, Holmes C W. 2000. Last interglacial reef growth beneath Belize barrier and isolated platform reefs. Geology, 28(5): 387-390.
[48]Grammer G M, Harris P M, Eberli G P. 2001. Carbonate platforms: Exploration-and production-scale insight from modern analogs in the Bahamas[J]. The Leading Edge, 20(3): 252-261.
[49]Haas J. 1999. Genesis of Late Cretaceous toe-of-slope breccias in the Bakony Mts, Hungary. Sedimentary Geology, 128(1): 51-66.
[50]Handford C R & Loucks R G. 1993. Carbonate depositional sequences and systems tracts- responses of carbonate platforms to relative sea-level changes. In: Carbonate Sequence Stratigraphy: Recent Developments and Applications (Ed. by Loucks R J & Sarg J F), AAPG Bulletin, 57, 3-41.
[51]Harris P M & Vlaswinkel M B. 2009. Modern isolated carbonate platforms: templates for quantifying facies attributes of hydrocarbon reservoirs. In: Controls on Carbonate Platform and Reef Development (Ed. by Lukasik J & Simo J A), Tulsa: SEPM- Soc Sedimentary Geology, 89, 323-341.
[52]Hontzsch S, Scheibner C, Kuss J, Marzouk A M, Rasser M W. 2011. Tectonically driven carbonate ramp evolution at the southern Tethyan shelf: the Lower Eocene succession of the Galala Mountains, Egypt[J]. Facies, 57(1): 51-72.
[53]Husinec A & Jelaska V. 2006. Relative sea-level changes recorded on an isolated carbonate platform: Tithonian to Cenomanian succession, southern Croatia[J]. Journal of Sedimentary Research, 76(9-10): 1120-1136.
[54]Husinec A & Read J F. 2011. Microbial laminite versus rooted and burrowed caps on peritidal cycles: Salinity control on parasequence development, Early Cretaceous isolated carbonate platform, Croatia[J]. Geological Society of America Bulletin, 123(9-10): 1896-1907.
[55]Isern A, McKenzie J, Feary D. 1996. The role of sea-surface temperature as a control on carbonate platform development in the western Coral Sea[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 124(3): 247-272.
[56]James, N. 1997. The cool-water carbonate depositional realm[J]. Special Publication-SEPM, 56: 1-22.
[57]Jones G D, Xiao Y T. 2006. Geothermal convection in the Tengiz carbonate platform, Kazakhstan: Reactive transport models of diagenesis and reservoir quality[J]. AAPG Bulletin, 90(8): 1251-1272.
[58]Jorry S J, Droxler A W, Francis J M. 2010. Deepwater carbonate deposition in response to re-flooding of carbonate bank and atoll-tops at glacial terminations[J]. Quaternary Science Reviews, 29(17-18): 2010-2026.
[59]Korte C, Kozur H W, Joachimski M M, Strauss H, Veizer J, Schwark L. 2004. Carbon, sulfur, oxygen and strontium isotope records, organic geochemistry and biostratigraphy across the Permian/Triassic boundary in Abadeh, Iran[J]. International Journal of Earth Sciences, 93(4): 565-581.
[60]Krull E S, Lehrmann D J, Druke D, Kessel B, Yu Y Y, Li R X. 2004. Stable carbon isotope stratigraphy across the Permian–Triassic boundary in shallow marine carbonate platforms, Nanpanjiang Basin, south China[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 204(3): 297-315.
[61]Kürschner W, Becker R T, Buhl D, Veizer J. 1992. Strontium isotopes in conodonts: Devonian-Carboniferous transition, the northern Rhenish Slate Mountains, Germany[J]. Ann. Soc. Géol. Belgique, 115(2): 595-621.
[62]Lees A. 1975. Possible influence of salinity and temperature on modern shelf carbonate sedimentation[J]. Marine Geology, 19(3): 159-198.
[63]Lehrmann D J, Payne J L, Felix S V, Dillett P M, Wang H, Yu Y Y, Wei J Y. 2003. Permian-Triassic boundary sections from shallow-marine carbonate platforms of the Nanpanjiang Basin, south China: Implications for oceanic conditions associated with the end-Permian extinction and its aftermath[J]. Palaios, 18(2): 138-152.
[64]Lehrmann D J, Pei D H, Enos P, Minzoni M, Ellwood B B, Orchard M J, Zhang J Y, Wei J Y, Dillett P, Koeni J, Steffen K, Druke D, Druke J, Kessel B, Newkirk T. 2007. Impact of differential tectonic subsidence on isolated carbonate-platform evolution: Triassic of the Nanpanjiang Basin, south China[J]. AAPG Bulletin, 91(3): 287-320.
[65]Li X W, Yu M Y, Lehrmann D J, Payne J L, Kelley B M, Minzoni M. 2012. Factors controlling carbonate platform asymmetry: Preliminary results from the Great Bank of Guizhou, an isolated Permian-Triassic Platform in the Nanpanjiang Basin, south China[J]. Palaeogeography Palaeoclimatology Palaeoecology, 315-316: 158-171.
[66]Lü C, Wu S, Yao Y,. Fulthorpe C S. 2013. Development and controlling factors of Miocene carbonate platform in the Nam Con Son Basin, southwestern South China Sea[J]. Marine and Petroleum Geology, 45: 55-68.
[67]Machel H G & Hunter I G. 1994. Facies models for Middle to Late Devonian shallow-marine carbonates, with comparisons to modern reefs: a guide for facies analysis[J]. Facies, 30(1): 155-176.
[68]Meyers S R. 2008. Resolving Milankovitchian controversies: The Triassic Latemar Limestone and the Eocene Green River Formation [J]. Geology, 36(4): 319-322.
[69]McNeill D F, Ginsburg R N, Chang S B R, Kirschvink J L. 1988. Magnetostratigraphic dating of shallow-water carbonates from San Salvador, Bahamas [J]. Geology, 16(1): 8-12.
[70]Minero C J. 1991. Sedimentation and diagenesis along open and island-protected windward carbonate platform margins of the Cretaceous El Abra Formation, Mexico[J]. Sedimentary Geology, 71(3): 261-288.
[71]Mitchum R M & Van Wagoner J C. 1991. High-frequency sequences and their stacking patterns: sequence-stratigraphic evidence of high-frequency eustatic cycles[J]. Sedimentary Geology, 70(2): 131-160.
[72]Mullins H T, Dolan J, Breen N, Andersen B, Gaylord M, Petruccione J L, Wellner R W, Melillo A J, Jurgens A D. 1991. Retreat of carbonate platforms: Response to tectonic processes[J]. Geology, 19(11): 1089-1092.
[73]Mutti M & Hallock P. 2003. Carbonate systems along nutrient and temperature gradients: some sedimentological and geochemical constraints[J]. International Journal of Earth Sciences, 92(4): 465-475.
[74]Navarro V, Ruiz-Ortiz P A, Molina J M. 2012. Birth and demise of a Middle Jurassic isolated shallow-marine carbonate platform on a tilted fault block: Example from the Southern Iberian continental palaeomargin[J]. Sedimentary Geology, 269-270, 37-57.
[75]Paterson R J, Whitaker F F, Jones G D, Smart P L, Waltham D, Felce G. 2006. Accommodation and sedimentary architecture of isolated icehouse carbonate platforms: Insights from forward modeling with CARB3D(+)[J]. Journal of Sedimentary Research, 76(9-10): 1162-1182.
[76]Payne J L, Summers M, Rego B L, Altiner D, Wei J Y, Yu M Y, Lehrmann D J. 2011. Early and Middle Triassic trends in diversity, evenness, and size of foraminifers on a carbonate platform in south China: implications for tempo and mode of biotic recovery from the end-Permian mass extinction[J]. Paleobiology, 37(3): 409-425.
[77]Pomar L. 2001a. Ecological control of sedimentary accommodation: evolution from a carbonate ramp to rimmed shelf, Upper Miocene, Balearic Islands [J]. Palaeogeography Palaeoclimatology Palaeoecology, 175(1-4): 249-272.
[78]Pomar L. 2001b. Types of carbonate platforms: a genetic approach[J]. Basin Research, 13(3):313-334.
[79]Pomar L, Bassant P, Brandano M, Ruchonnet C, Janson X. 2012. Impact of carbonate producing biota on platform architecture: Insights from Miocene examples of the Mediterranean region. Earth-Science Reviews, 113(3-4): 186-211.
[80]Preto N, Hinnov L A, Hardie L A, De Zanche V. 2001. Middle Triassic orbital signature recorded in the shallow-marine Latemar carbonate buildup (Dolomites, Italy) [J]. Geology, 29(12): 1123-1126.
[81]Qiu Z, Wang Q C, Zou C N, Yan D T, Wei H Y. 2013. Transgressive–regressive sequences on the slope of an isolated carbonate platform (Middle–Late Permian, Laibin, South China)[J]. Facies, Springer-Verlag Berlin Heidelberg, DOI 10.1007/s10347-012-0359-4.
[82]Rankey E C, Rodrigo Garza-Perez J. 2012. Seascape metrics of shelf-margin reefs and reef sand aprons of Holocene carbonate platforms[J]. Journal of Sedimentary Research, 82(1-2): 53-71.
[83]Read J F. 1982. Carbonate platforms of passive (extensional) continental margins: types, characteristics and evolution[J]. Tectonophysics, 81(3): 195-212.
[84]Read J F. 1985. Carbonate platform facies models[J]. AAPG Bulletin, 69(1):1-21.
[85]Reijmer J J, Bauch T, Schäfer P. 2012. Carbonate facies patterns in surface sediments of upwelling and non‐upwelling shelf environments (Panama, East Pacific) [J]. Sedimentology, 59(1): 32-56.
[86]Ronchi P, Ortenzi A, Borromeo O, Claps M, Zempolich W G. 2010. Depositional setting and diagenetic processes and their impact on the reservoir quality in the late Visean-Bashkirian Kashagan carbonate platform (Pre-Caspian Basin, Kazakhstan) [J]. AAPG Bulletin, 94(9): 1313-1348.
[87]Ruppel S C & Ward W B. 2013. Outcrop-based characterization of the Leonardian carbonate platform in west Texas: Implications for sequence-stratigraphic styles in the Lower Permian[J]. AAPG Bulletin, 97(2): 223-250.
[88]Schafer P & Senowbari-Daryan B. 1981. Facies development and paleoecologic zonation of four Upper Triassic patch reefs, Northern Calcareous Alps near Salzburg, Austria. In: European reef models –Society of Economic Paleontologists and Mineralogists (Ed. by Toomey D F), Special Publications, 30, 241-259.
[89]Scheibner C, Marzouk A M, Kuss J. 2001. Shelf architectures of an isolated Late Cretaceous carbonate platform margin, Galala Mountains (Eastern Desert, Egypt)[J]. Sedimentary Geology, 145: 23-43.
[90]Scheibner C, Kuss J, Speijer R. 2003. Stratigraphic modelling of carbonate platform-to-basin sediments (Maastrichtian to Paleocene) in the Eastern Desert, Egypt[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 200(1): 163-185.
[91]Schlager W. 1999. Scaling of sedimentation rates and drowning of reefs and carbonate platforms[J]. Geology, 27(2): 183-186.
[92]Schlager W. 2003. Benthic carbonate factories of the Phanerozoic[J]. International Journal of Earth Sciences, 92(4): 445-464.
[93]Sun S Q, Esteban M. 1994. Paleoclimatic controls on sedimentation, diagnesis, and reservior quality: Lessons from Miocene carbonates[J]. AAPG Bulletin, 78(4): 519-543.
[94]Tucker M E. 1990. Geological background to carbonate sedimentation. In: Carbonate Sedimentology (Ed. by Tucker M E & Wright V P), Oxford(UK): Blackwell Scientic Publications, 28-69.
[95]van Geldern R, Joachimski M M, Day J, Jansen U, Alvarez F, Yolkin E A, Ma X P. 2006. Carbon, oxygen and strontium isotope records of Devonian brachiopod shell calcite[J]. Palaeogeography Palaeoclimatology Palaeoecology, 240(1-2): 47-67.
[96]Veizer J, Buhl D, Diener A, Ebneth S, Podlaha O G, Bruckschen P, Jasper T, Korte C, Schaaf M, Ala D. 1997. Strontium isotope stratigraphy: potential resolution and event correlation[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 132(1): 65-77.
[97]Vera J, Molina J, Montero P, Bea F. 1997. Jurassic guyots on the Southern Iberian Continental Margin: a model of isolated carbonate platforms on volcanic submarine edifices[J]. Terra Nova, 9(4): 163-166.
[98]Verwer K, Merino-Tomé O, Kenter J A, Della Porta G. 2009. Evolution of a high-relief carbonate platform slope using 3D digital outcrop models: Lower Jurassic Djebel Bou Dahar, High Atlas, Morocco[J]. Journal of Sedimentary Research, 79(6): 416-439.
[99]Warrlich G, Bosence D, Waltham D, Wood C, Boylan A, Badenas B. 2008. 3D stratigraphic forward modelling for analysis and prediction of carbonate platform stratigraphies in exploration and production. Marine and Petroleum Geology[J], 25(1): 35-58.
[100]Webb G E & Kamber B S. 2000. Rare earth elements in Holocene reefal microbialites: a new shallow seawater proxy[J]. Geochimica et Cosmochimica Acta, 64(9): 1557-1565.
[101]Wienberg C, Westphal H, Kwoll E, Hebbeln D. 2010. An isolated carbonate knoll in the Timor Sea (Sahul Shelf, NW Australia): facies zonation and sediment composition[J]. Facies, 56(2): 179-193.
[102]Williams H D, Burgess P M, Wright V P, Della Porta G, Granjeon D. 2011. Investigating carbonate platform types: Multiple controls and a continuum of geometries[J]. Journal of Sedimentary Research, 81(1): 18-37.
[103]Wilson J L. 1975. Carbonate facies in geologic history[M]. New York: Springer Verlag Berlin.
[104]Wilson M E J. 2000. Tectonic and volcanic influences on the development and diachronous termination of a tertiary tropical carbonate platform[J]. Journal of Sedimentary Research, 70(2): 310-324.
[105]Wilson M E & Lokier S W. 2002. Siliciclastic and volcaniclastic influences on equatorial carbonates: insights from the Neogene of Indonesia[J]. Sedimentology, 49(3): 583-601.
[106]Wright V. 1992. Speculations on the controls on cyclic peritidal carbonates: ice-house versus greenhouse eustatic controls[J]. Sedimentary Geology, 76(1): 1-5.
[107]Wright V P & Burchette T P.1996. Shallow-water carbonate sediments. In: Sedimentary environments: processes, facies and stratigraphy(Ed. by Reading H G), Oxford (UK): Blackwell Science, 325-394.
[108]Wright V P & Burgess P M. 2005. The carbonate factory continuum, facies mosaics and microfacies: an appraisal of some of the key concepts underpinning carbonate sedimentology[J]. Facies, 51(1-4): 17-23.
[109]Wright V, Vanstone S. 2001. Onset of Late Palaeozoic glacio-eustasy and the evolving climates of low latitude areas: a synthesis of current understanding[J]. Journal of the Geological Society, 158(4): 579-582.
[110]Yang W, Lehrmann D J. 2003. Milankovitch climatic signals in Lower Triassic (Olenekian) peritidal carbonate successions, Nanpanjiang basin, South China[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 201(3): 283-306.
[111]Zamagni J, Mutti M, Ballato P, Košir A. 2012. The Paleocene–Eocene thermal maximum (PETM) in shallow-marine successions of the Adriatic carbonate platform (SW Slovenia)[J]. Geological Society of America Bulletin, 124(7-8): 1071-1086.
[112]Zampetti V, Schlager W, van Konijnenburg J-H, Everts A-J. 2004. Architecture and growth history of a Miocene carbonate platform from 3D seismic reflection data; Luconia province, offshore Sarawak, Malaysia[J]. Marine and Petroleum Geology, 21(5): 517-534.
[113]Zühlke R, Bechstädt T, Mundil R. 2003. Sub-Milankovitch and Milankovitch forcing on a model Mesozoic carbonate platform-the Latemar (Middle Triassic, Italy) [J]. Terra Nova, 15(2): 69-80.
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