首页> 外文会议>Convention of the Gulf Coast Association of Geological Societies American Association of Petroleum Geologists Sectional Meeting;Meeting of the Gulf Coast Section of the Society of Economic Paleontologists and Mineralogists >Correlation of Events for the Jurassic and Cretaceous of the Northern Gulf of Mexico Margin Using Mega-Regional Onshore/Offshore-Composited PSDM Seismic Grid
【24h】

Correlation of Events for the Jurassic and Cretaceous of the Northern Gulf of Mexico Margin Using Mega-Regional Onshore/Offshore-Composited PSDM Seismic Grid

机译:墨西哥境内北海岸北海岸/海上船舶近海岸边侏罗纪和白垩纪事件的相关性

获取原文

摘要

Our Gulf of Mexico interpretation shows a new depth map of the mid-Jurassic unconformity at base Louann Salt ranging throughout the Gulf of Mexico Basin. A gradient calculation highlights distinct flexures that separate the historic onshore basins and uplifts. The flexures fan out from southwest to northeast in a pattern consistent with the pull-apart of Africa and Florida, proposing a new view of the basement framework. There is abundant evidence of old Louann Salt movement in the onshore, offshore and deepwater, caused by gravity forces. Onshore growth wedges are numerous in Smackover, Lower Cotton Valley age. Offshore old salt stocks formed in deepwater and show a thinned Mesozoic section. The stocks were squeezed and salt evacuated, and the Mesozoic thinned section has been drilled in suprasalt canopy positions in numerous offshore locations. In the deep-water environment, a regional Jurassic-age salt nappe extruded over a more northerly position for the continental/oceanic boundary. Florida events seem to correlate with basement movement in the onshore Gulf margin. A second stage rift event interpreted at a Lower Cretaceous unconformity in the southwest Florida shelf region, suggests correlation with Mesozoic basement movements in the onshore uplifts. The Middle to Upper Jurassic shelf edges are regionally interpreted and assist in reconstruction of the early onshore basins to the Florida shelf. Interpretation of the Gulf of Mexico Basin framework has long been hindered by the separation of datasets west to east and onshore to offshore. This is addressed by a unique pre-stack depth migration (PSDM) onshore and offshore grid of dip and strike composite seismic lines that range from the Texas/Mexico border to the Florida Panhandle, and from the onshore shelf margins to the deepwater abyssal plain. This seamless mega-regional grid is unique to any margin in the world today, and offers advanced correlation of events around the Gulf of Mexico Basin, especially the Jurassic and Cretaceous history.
机译:我们的墨西哥湾的解释显示了在墨西哥盆地湾的基地Louann盐的中侏罗桑斯不整合的新深度地图。渐变计算突出了不同历史陆上盆地和隆起的不同的柔性。在与非洲和佛罗里达州的拉开的外在往复的模式中,柔性扇子从西南到东北部门的粉丝。陆上,近海和深水的旧洛南盐运动有丰富的证据。陆上增长楔子众多棉花谷时代众多。海上老盐股在深水中形成,表现出薄薄的中生代部分。股票被挤压,盐疏散,中生代稀薄部分已经在众多海上地点的Suprasalt Canopy位置钻探。在深水环境中,一个区域侏罗纪盐纳皮布在欧洲/海洋边界的更北极地位置挤出。佛罗里达州的事件似乎与陆上海湾边缘的地下室运动相关。在佛罗里达州西南部的较低白垩纪不整合处解释的第二阶段Rift事件表明与陆上隆起的中生代地下室运动相关联。区域到上部侏罗纪货架边缘被区域解释并协助重建陆上盆地早期盆地到佛罗里达州。墨西哥湾博物馆的解释长期以来一直阻碍了西部到东部和陆上到海上的数据集。这是由独特的堆叠深度迁移(PSDM)陆上和海上网格的倾角和罢工复合地震线的陆上网格来解决,这些线条从德克萨斯州/墨西哥边境到佛罗里达队的边界,以及从陆上货架边距到深水深海平原。这个无缝的巨型区域网格今天是世界上任何余量的独有,并提供墨西哥湾盆地湾周围的事件的高级相关性,特别是侏罗纪和白垩纪历史。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号