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Phanerozoic paleogeography,paleoenvironment and lithofacies maps of the circum-Atalantic margins

机译:环大西洋大西洋边缘的古生代古地理,古环境和岩相图

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A series of maps was constructed,depicting the plate tectonic configuration,paleogeography,baleoenvironment and lithofacies for Phanerozoic time intervals from Cambrian through the Neogene.These are world maps comprising 300 continental plates and terranes,but are reprojected here to illustrate the circum-Atlantic margins.The relative jpositin of the continents through time was largely derived from Plates and PALEOMAP software.These maps illusrate the JPhanerozoic geodynamic evolutin of hte Earth.They show the relationship of the continental configuration,lithofacies,tectonics,and climate,from the time of hte diassembly of Rodinia to the assembly and break-up of Pangea.From a regional perspective,the facies in basins along the circum-Atlantic margin reflect various stages of rifting and passive margin development.Inversio caused by ridge push played an important role in the basin evolutin and has influenced the distribution of lithofacties at various times.The power of the maps is realized in their application as an aid to the visualization of the relationship of regional basin development,sedimentation and erosion to the deposition of potential source-rock,reservoir and seals.The individual maps illustrate the conditions present during the maximum marine transgressions of sea-level within the Sauk,Tippecanoe,Kaskaskia,Absaroka,Zuni,and Tejas megasequences of Sloss.Relative sea level cyclicity,chronostratigraphy,and regional unconformities provide the basis for partitioning these higher frequency depositional cycles into 32 subdivisions (supersequences) ranging in duratio from 11 to 39 my.In this report 14 of these time slices are used to illustrate the environments and lithologies resulting from changes in the geographic position of the terranes which constitute the present Atlantic margins.The text attempts to fill in details of the progressive change between mapped intervals.Data for the maps were derived from geologic reports,maps and stratigraphic columns adn other paleogeographic interpretations regarding tectonics,basin formation,and deposition.The lithofacies are depicted by 21 patterns.
机译:绘制了一系列地图,描述了从寒武纪到新近纪的古生代时间间隔的板块构造构造,古地理,古环境和岩相。这些世界地图包含300个大陆板块和地形,但在此处进行了重新投影以说明大西洋周围的边界随时间变化的大陆相对沉积物主要来自Plates和PALEOMAP软件。这些地图说明了地球的JP代生代动力学动力学演化。它们显示了自Ht时代以来大陆构造,岩相,构造和气候之间的关系。从区域角度来看,沿大西洋-大西洋边缘的盆地相反映了裂谷作用和被动边缘发育的各个阶段。脊推引起的逆作用在盆地中起着重要作用。 evolutin并在不同时间影响岩相分布。地图的力量是真实的在其应用中进行了改进,以帮助可视化区域盆地发育,沉积和侵蚀与潜在烃源岩,储层和海豹沉积的关系。单个地图显示了海平面在最大海侵期间存在的条件在Sauk,Tippecanoe,Kaskaskia,Absaroka,Zuni和Tejas的Sloss巨型序列中。相对的海平面周期性,年代地层学和区域不整合面为将这些较高频率的沉积周期划分为32个细分(超序列)提供了基础,这些细分范围从11到11 39 my。在本报告中,这些时间片中的14个用于说明由构成当前大西洋边缘的地层的地理位置变化而导致的环境和岩性。本文试图填写映射区间之间的渐进式变化的详细信息地图数据来自地质报告,地图和地层列及有关构造,盆地形成和沉积的古地理解释。岩相由21种模式描绘。

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