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首页> 外文期刊>AAPG Bulletin >Regional structural setting and evolution of the Mississippi Canyon, Atwater Valley, western Lloyd Ridge, and western DeSoto Canyon protraction areas, northern deep-water Gulf of Mexico
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Regional structural setting and evolution of the Mississippi Canyon, Atwater Valley, western Lloyd Ridge, and western DeSoto Canyon protraction areas, northern deep-water Gulf of Mexico

机译:密西西比峡谷,亚特谷,劳埃德岭西部峡谷峡谷峡谷峡谷峡谷区的区域结构环境和演变,墨西哥北部深水湾

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摘要

The structural framework and evolution from the Middle Jurassic to the present of the Mississippi Canyon, Atwater Valley, western DeSoto Canyon, and western Lloyd Ridge protraction areas consist of a complex history influenced by basement fabric, multiple stages of salt movement, and gravitational gliding. A detailed tectono-stratigraphic interpretation of the study area indicates that three main stages of salt movement controlled sediment dispersal patterns and the formation and evolution of intraslope minibasins. These three stages of salt movement occurred during the Cretaceous, the Paleogene, and the Neogene.
机译:从中间侏罗纪到目前袭峡谷,阿斯图斯谷,西部峡谷和西方劳埃德山脊突起区域的结构框架和演变由一个受地下织物的复杂历史,盐运动多个阶段和引力滑动。 研究区的详细构造 - 地层解释表明盐运动的三个主要阶段控制了沉积物分散模式以及肿瘤内含有肿瘤的形成和演化。 在白垩纪,古烯和新生儿中发生了这三个阶段的盐运动。

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