...
首页> 外文期刊>Marine and Petroleum Geology >Tectonic control of the oil-rich large igneous-carbonate-salt province of the South Atlantic rift
【24h】

Tectonic control of the oil-rich large igneous-carbonate-salt province of the South Atlantic rift

机译:南大西洋裂谷富含石油的大型火成碳酸盐岩省的构造控制

获取原文
获取原文并翻译 | 示例
           

摘要

The Early Cretaceous South Atlantic Magmatic Province (SAMP), which includes the Parana-Etendeka LIP, produced about 8 million km(3) of tholeiitic basalt and diabase over an area of 4 million km(2). Huge pre-salt oil reserves, discovered in 2007 by Petrobras in non-marine carbonates, are estimated at more than 45 billion barrels. Here we show the close causal relationship of the southward increasing width of the wedge-shaped South Atlantic rift with the similarly southward increase in igneous activity, in the thicknesses of non-marine carbonate and salt, and in the size of oil reserves, all controlled mainly by South America's early clockwise rotation away from Africa about a pole in its northeast. Large diabase dike swarms transversal to the rift witness to South America's rotation that opened in its wake the southward widening South Atlantic rift. Westward increasing pressure on the Equatorial margin by South America's clockwise rotation forced open the Benue trough and created pre-late-Aptian folds in the Demerara Plateau and in Brazil's Solimoes (Upper Amazonas) basin. Prerift and synrift volcanic activity increases southward, culminating in the Parana-Etendeka LIP and in the offshore volcanic SDRSs that continue southward to the Cape Basin. Berriasian-Valanginian rift sediments deposited from about 145 Ma, 10 Ma before the flood basalts of the Parana-Etendeka LIP. The largest transversal dike swarm continued in the proto-Walvis Ridge that separated the central South Atlantic endorheic rift basin from the sea in the south; erosion and leaching of basalts supplied Ca, Mg, and SiO2 to the endorheic basin for the deposition of non-marine carbonates and authigenic clays. Basalt flows intercalated with carbonates nearly until salt deposition about 113 Ma. Hypogenic leaching of carbonates by mantle-derived CO2 created optimal reservoirs. Supergiant oil deposits occur where the widest endorheic basin and the volcanic province overlap. (C) 2016 Elsevier Ltd. All rights reserved.
机译:包括Parana-Etendeka LIP在内的早白垩世南大西洋岩浆岩省(SAMP)在400万平方公里(2)的面积中产生了约800万平方公里的玄武岩和辉绿岩。巴西国家石油公司(Petrobras)于2007年在非船用碳酸盐中发现了巨大的盐下石油储量,估计超过450亿桶。在这里,我们显示了楔形南大西洋裂谷向南增加的宽度与火成活动的向南增加,非海洋碳酸盐和盐的厚度以及石油储量的大小之间的紧密因果关系,所有这些都受到控制主要是由于南美洲早先沿顺时针方向从非洲绕其东北的一极旋转。辉绿岩大堤汇聚到裂谷的见证处,见证了南美向南扩展的南大西洋裂谷的旋转。南美顺时针旋转使赤道边缘向西增加的压力迫使贝努尔海槽打开,并在德梅拉拉高原和巴西的Solimoes(亚马逊河上游)盆地中形成了晚期Apt褶皱。预裂和合裂的火山活动向南增加,最终在巴拉那-埃滕德卡LIP和向南延伸到开普盆地的近海火山SDRS中。 Berriasian-Valanginian裂谷沉积物沉积于Parana-Etendeka LIP的洪水玄武岩之前约145 Ma,10 Ma。最大的横向堤防群继续在原沃尔维斯山脊中,该中脊将南大西洋中性背胶裂谷盆地与南部海区分开;玄武岩的侵蚀和浸出将钙,镁和SiO2输送到背胶盆地,以沉积非海洋碳酸盐和自生粘土。玄武岩流几乎与碳酸盐夹层,直到盐沉积约113 Ma。地幔衍生的二氧化碳对碳酸盐的低渗作用创造了最佳的储层。超大型油藏发生在最宽的背胶盆地与火山省重叠的地方。 (C)2016 Elsevier Ltd.保留所有权利。

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