The research progress of lithofacies paleogeography in China
-
摘要: 我国的岩相古地理研究大致经历了三个大的发展时期。初期阶段：20世纪80年代以前，主体是以古生物地层学的理论为指导编制出版大区域的古地理图集，集中反映海陆分布，岩相内容较少，较少的学者开展了岩相古地理研究，揭开了由古地理图向岩相古地理图转变的序幕。快速发展阶段：20世纪80年代至2000年，总体上是以大地构造学、古生物地层学、沉积学等理论为指导，开展了大量的岩相古地理研究与编图工作，并采取多种编图思路和方法编制大区域的岩相古地理图，是我国岩相古地理研究与编图大发展时期，形成了丰硕的理论和实践成果。编制的图件不仅尽量体现活动性古地理的学术前沿，而且更多的是强化实用性，聚焦对沉积层控矿产远景预测和油气勘探的支撑和指导作用。现代阶段：2000年至今，岩相古地理研究与编图聚焦支撑油气地质调查与勘探成为了这段时间的主题，采取不同的编图思路和方法编制出版了大区域的岩相古地理图。具有三大特点：一是编图资料丰富，技术方法新颖；二是编图思路先进，体现了以构造为主线，岩相古地理恢复为核心，支撑服务油气为根本的研究思路；三是以服务油气目标为特色。由于大数据、人工智能等信息技术突飞猛进促进大数据岩相古地理向前发展，数字岩相古地理必将推动我国在岩相古地理编图思路和技术方法的创新，提升支撑服务沉积矿产找矿和油气勘探开发的精准性和预测性水平。Abstract: The study of lithofacies paleogeography in China has experienced three stages of development.Early stage:before the 1980s.The main subjects were the paleogeographic atlas of a large area under the theoretical guidance of paleontology stratigraphy, which more reflected the distribution of sea and land. The content of lithofacies was less. A few scholars had carried out the study of lithofacies paleogeography, which opened the prelude of the transformation from paleogeographic map to lithofacies paleogeography map.Rapid development stage:1980s to 2000.Overall in geotectonics, palaeontologic stratigraphy and sedimentology theory as the instruction, a large number of lithofacies palaeogeographic research and mapping works with a variety of mapping thoughts and methods had been carried out, and lithofacies paleogeographic maps of large area have been completed. It was a period of great development of lithofacies palaeogeography and mapping in China, fruitful theoretical and practical achievements had been produced in this stage. These maps not only reflected the academic frontier of active paleogeography, but also strengthened the practicability. Furthermore, the support and guidance of prospect prediction in sedimentary mineral and oil-gas exploration was focused on.Modern stage:2000 to present.Lithofacies palaeogeography research and mapping focusing on supporting oil and gas geological survey and exploration has become the theme in this period, different mapping thoughts and methods have been applied to these lithofacies palaeogeography maps of large areas. There are three main characteristics:first, abundant mapping data and novel technical methods has been used. The second is the advanced mapping idea, which reflects the research idea of tectonics as the main line and restoration of lithofacies paleogeography as the core, and the support of oil and gas exploration as the fundamental.Third, it is characterized by targets on service of oil and gas exploration.Because of the rapid advances in big data, artificial intelligence and other information technology, the development of big data lithofacies palaeogeography has also propelled forward.The digital lithofacies palaeogeography will certainly promote the innovation in mapping ideas and technical methods of lithofacies palaeogeography in China, which can improve the accuracy and predictability of sedimentary mineral prospecting and oil and gas exploration and development.
-
-
Folk R L, 1965.Henry Clifton Sorby (1826-1908), founder of petrography[J].Journal of Geological Education, 13(2):43-47.
Krumbein W C, SlossLL, 1963.Stratigraphy and sedimentation[M].2nd edtion.San Franscisco:Freeman, 1-660.
Miall A D, 1990.Principles of sedimentary basin analysis:introduction[M].Berlin, Heidelberg, New York, London, Paris, Tokyo, Hong Kong, Barcelona:Springer-Verlag.
Moore R C, 1949.Meaning of facies[C].In:Longwell C R(ed).Sedimentary facies in geological history[A].The Geological Society of America Memoir,39:1-34.
Pettijohn F J, 1975.Sedimentary rocks (Third edition)[M].New York:Harper and Row Inc.628.
Pettijohn F J,1962.Paleocurrents and paleogeography[J].AAPG Bulletin,46(8):1468-1493.
Pitman W C, 1978.Relationship between eustasy and stratigraphic sequence of passive margins[J].Geological Soceity of America Bulletin, 89(9):1389-1403.
Posamentier H W,1988.Eustatic controls on clastic deposition, I-conceptual framework[J].SEPM Special Publication, 42.
Potter P E,1967.Sand bodies and sedimentary environments, a review[J].AAPG Bulletin, 51(3):337-365.
Potter P E, Pettijohn F J, 1963.Paleocurrents and basin analysis[M].New York:Springer,296.
Sarg J F, 1988.Carbonate sequence stratigraphy.//Sea-Level Changes-An Integrated Approach[G].SEPM Special Publication,42:155-181.https://doi.org/10.2110/pec.88.01.0155
Selley R C, 1970.Ancient sedimentary environments[M].Ithaca New York:Cornell University Press:237.
Selley R C, 1976.An introduction to sedimentology[M].London:Acadymic Press.
Shepard F P, Moore D G, 1955.Central Texas coast sedimentation characteristics of sedimentary environment, recent history and diagenesis[C].Sedimentology of South Texas Field Trip Guidebook, 95-97.
Sloss L L, Dapples E C,Krumbein W C, 1960.Lithofacies maps:An atlas of the United States and southern Canada[M].New York:Wiley, 1-108.
Sloss J F, 1988.Forty years of sequence stratigraphy[J].Geological Society of America Bulletin,100(11):1661-1665.
Sorby H C, 1857.On the physical geography of the Tertiary estuary of the Isle of Wight[J].Quarterly Journal of the Geological Society(1-2):137-138.
Sorby H C,1859.On the structures produced by the current present during the deposition of stratified rocks[J].Geologist, 2:137-147.
Sorby H C,1879.On the structure and origin of limestones (presential address.1879)[J].Proceedings of the Geological Society of London,35,56-95.
Sorby H C,1880.On the structure and origin of non-calcareous stratified rocks (presential address.1879)[J].Proceedings of the Geological Society of London,36:.46-92.
Twenhofel W H, 1950.Principles of sedimentation[M].New York:McGraw-Hill Co.[KG-*4],1-673.
Vail P R, 1987.Seismic stratigraphy interpretation using sequence stratigraphy, Part 1:Seismic stratigraphy interpretation procedure[J].AAPG Memoir, 36:129-144.
Van Wagoner J E, Posamentier H W, Mitchum R M, et al.[KG-*4], 1988.An overview of the fundamentals of sequence stratigraphy and key definitions[M].SEPM Special Publication.
曾允孚,夏文杰,1986.沉积岩石学[M].北京:地质出版社.
地科院情报研究所编译.1975.岩相古地理研究及编图方法[M].1-291.
冯增昭,1989.碳酸盐岩岩相古地理学[M].北京:石油工业出版社.
冯增昭,1993.沉积岩石学[M].北京:石油工业出版社.
关士聪,1984.中国海陆变迁海域沉积相与油气[M].北京:科学出版社.
何镜宇,孟祥化,1987.沉积岩和沉积相模式及建造[M].北京:地质出版社.
李耀西,1975.大巴山西段早古生代地层志[M].北京:地质出版社.
里丁HG,1985.沉积环境和相[M].周明鉴等,译.北京:科学出版社.
刘宝珺,1980.沉积岩石学[M].北京:地质出版社.
刘宝珺,曾允孚,1985.岩相古地理基础和工作方法[M].北京:地质出版社.
刘宝珺,许效松,1994.中国南方岩相古地理图集[M].北京:科学出版社.
刘鸿允,1955.中国古地理图[M].北京:科学出版社.
卢衍豪,1965.中国寒武纪岩相古地理轮廓初探[J].地质学报,45(4):349-357.
鲁欣,张介涛译,1953.沉积岩石学原理(中册)[M].北京:地质出版社.
马永生,陈洪德,王国力,2009.中国南方构造-层序地层岩相古地理图集(震旦纪-新近纪)[M].北京:科学出版社.
马永生,牟传龙,郭旭升,等, 2006b.Sedimentary facies and distribution of the reservoir rocks from the Feixianguan Formation in the Daxian-Xuanhan region, northeastern Sichuan[J].Acta Geologica Sinica, 80(1):137-151.
马永生,牟传龙,郭旭升,等,2006a.川东北地区长兴组沉积特征与沉积格局.地质论评,52(1):25-29.
牟传龙,马永生,谭钦银,等,2007.四川通江-南江-巴中地区长兴组-飞仙关组沉积模式[J].地质学报,81(6):820-826.
牟传龙,丘东洲,王立全,等,2000.湘鄂赣二叠系层序岩相古地理与油气[M].北京:地质出版社.
牟传龙,王启宇,王秀平,等,2016a.岩相古地理研究可作为页岩气地质调查之指南[J].地质通报,35(1):10-19.
牟传龙,王启宇,王秀平,等,2016b.造山带岩相古地理研究与实践[J].沉积学报,34(1):1-14.
牟传龙,王秀平,王启宇等,2017.岩相古地理与页岩气地质调查[M].北京:科学出版社.
牟传龙,许效松,2010.华南地区早古生代沉积演化与油气地质条件[J].沉积与特提斯地质,30(3):24-29.
牟传龙,许效松,林明,1992.层序地层与岩相古地理编图——以华南泥盆纪为例[J].岩相古地理,10(4):1-9.
牟传龙,周恳恳,陈小炜等,2016.中国岩相古地理图集(埃迪卡拉纪-志留纪)[M].北京:地质出版社.
牟传龙,马永生,谭钦银,等,2007.四川通江-南江-巴中地区长兴组-飞仙关组沉积模式.地质学报,81(6):820-826.
牟传龙,2022.关于相的命名及其分类的建议[J/OL].沉积与特提斯地质, 42(3):331-339.https://doi.org/10.19826/j.cnki.1009-3850.2022.03001
米哈伊洛 H A,1973.大比例尺岩相图及古地理图的编制方法[M].//岩相古地理研究及编图方法.北京:地质科学研究院情报研究所,1975.
纳利夫金B Д,等,1963.编制俄罗斯地台及其边缘地槽区岩相图和古地理图的基本原则[M].//岩相古地理研究及编图方法.北京:地质科学研究院情报研究所,1975.
王鸿祯,1985.中国古地理图集[M].北京:地图出版社.
王秀平,牟传龙,王启宇,等,2018.论岩相古地理可作为页岩气地质调查之指南[J].沉积学报,36(2):215-231.
许效松,1999.古地理研究的前景与挑战[J].古地理学报,1(4):1-11.
许效松,牟传龙,林明,1993.露头层序地层与华南泥盆纪古地理[M].成都:成都科技大学出版社.
叶德胜,等,1983.贵州泥盆纪碳酸盐岩沉积相[J].沉积学报,1(2):84-95.
余素玉,何镜宇,1989.沉积岩石学[M].北京:地质出版社.
郑和荣,胡宗全,2000.中国前中生代构造-岩相古地理图集[M].北京:地质出版社.
周恳恳,牟传龙,许效松,等, 2014.华南中上扬子早志留世古地理与生储盖层分布[J].石油勘探与开发, 41(5):623-633.
-
计量
- 文章访问数: 885
- PDF下载数: 44
- 施引文献: 0
下载: