Phanerozoic paleogeography,paleoenvironment and lithofacies maps of the circum-Atlantic margins |
| |
| Institution: | 1. Department of Earth and Planetary Systems Science, Hiroshima University, 1-3-1 Kagamiyama, Higashihiroshima, Hiroshima 739-8526, Japan;2. Faculty of Culture and Education, Saga University, 1 Honjo-Machi, Saga 840-8502, Japan;3. Center for Advanced Marine Core Research, Kochi University, Kochi 783-8502, Japan;4. Department of Earth and Planetary Science, The University of Tokyo, 7-3-1 Hongo, Bunkyo-ku, Tokyo 113-0033, Japan;1. Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY 10964, USA;2. Earth and Planetary Sciences, Rutgers University, Piscataway, NJ 08854, USA;3. Dipartimento di Scienze della Terra ''Ardito Desio'', Università degli Studi di Milano, via Luigi Mangiagalli 34, I-20133, Milan, Italy;1. GeoZentrum Nordbayern, Universität Erlangen-Nürnberg, Schlossgarten 5, 91054 Erlangen Germany;2. Department of Geological Sciences, University of Texas at San Antonio, One UTSA Circle, San Antonio, TX 78249, USA |
| |
| Abstract: | A series of maps was constructed, depicting the plate tectonic configuration, paleogeography, paleoenvironment 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 position of the continents through time was largely derived from PLATES and PALEOMAP software.These maps illustrate the Phanerozoic geodynamic evolution of the Earth. They show the relationship of the continental configuration, lithofacies, tectonics, and climate, from the time of the disassembly 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. Inversion caused by ridge push played an important role in the basin evolution and has influenced the distribution of lithofacies 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 duration 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 and other paleogeographic interpretations regarding tectonics, basin formation, and deposition. The lithofacies are depicted by 21 patterns. |
| |
| Keywords: | |
| 本文献已被 ScienceDirect 等数据库收录！ |
|
