首页> 外文期刊>Aeolian research >Origins of late- Pleistocene coastal dune sheets, Magdalena and Guerrero Negro, from continental shelf low-stand supply (70-20 ka), under conditions of southeast littoral- and eolian-sand transport, in Baja California Sur, Mexico
【24h】

Origins of late- Pleistocene coastal dune sheets, Magdalena and Guerrero Negro, from continental shelf low-stand supply (70-20 ka), under conditions of southeast littoral- and eolian-sand transport, in Baja California Sur, Mexico

机译:来自欧洲欧式货架低销供应(70-20 kA),在东南沿岸和烧沙运输的条件下,在Baja California Sur,墨西哥的条件下,Magdalena和Guerrero Negro的起源

获取原文
获取原文并翻译 | 示例
           

摘要

Shallow morpho-stratigraphic sections (n = 11) in each of two large coastal dune sheets including the Magdalena (7000 km(2)) and Guerrero Negro (8000 km(2)) dune sheets, from the Pacific Ocean side of Baja California Sur, Mexico, have been analyzed for dune deposit age. The shallow morphostratigraphic sections (similar to 2-10 m depth) include 11 new TL and C-14 ages, and paleosol chronosequences, that differentiate cemented late Pleistocene dune deposits (20.7 +/- 2.1 to 99.8 +/- 9.4 ka) from uncemented Holocene dune deposits (0.7 +/- 0.05 to at least 3.2 +/- 0.3 ka). Large linear dune ridges (5-10 m in height) in the dune sheet interiors trend southeast and are generally of late Pleistocene age (similar to 70-201ka). The late Pleistocene dune deposits reflect eolian transport of marine sand across the emerged continental shelf (30-50 km southeast distance) from low-stand paleo-shorelines (-100 +/- 25 m elevation), which were locally oriented nearly orthogonal to modeled deep-water wave directions (similar to 300 TN). During the Holocene marine transgression, onshore and alongshore wave transport delivered remobilized shelf sand deposits to the nearshore areas of the large dune sheets, building extensive barrier islands and sand spits. Submerged back-barrier lagoons generally precluded marine sand supply to dune sheet interiors in middle to late Holocene time, though exceptions occur along some ocean and lagoon shorelines. Reactivation of the late Pleistocene dune deposits in the dune sheet interiors lead to generally thin (13 m thickness), but widespread, covers of Holocene dune deposits (0.41 +/- 0.05 to 10.5 +/- 1.6 ka). Mechanical drilling will be required to penetrate indurated subsoil caliche layers to reach basal Pleistocene dune deposits. (C) 2017 Elsevier B.V. All rights reserved.
机译:两个大沿海沙丘床单(包括Magdalena(7000公里(2))和Guerrero Negro(8000公里(2))的沙丘床单,来自Baja California Sur的太平洋床,墨西哥已被分析为沙丘存款年龄。浅层的情况(类似于2-10米深度)包括11个新的T1和C-14岁,以及古溶胶慢性核糖,从未发布全新世沙丘沉积(0.7 +/- 0.05至至少3.2 +/- 0.3 ka)。沙丘片内部趋势东南的大线性沙丘脊(高度为5-10米),通常是晚熟年龄(类似于70-201KA)。迟到的更新世沙丘沉积物反映了海洋沙子的Eolian运输,跨越古老的陆地架(东南距离)从低立场古海岸(-100 +/- 25米海拔),这在局部导向与建模的局部正交深水波方向(类似于300 TN)。在全新世海运违规期间,陆上和沿岸波浪运输将重新化的货架砂存放到大沙丘床单的近岸地区,建立广泛的屏障群岛和沙子吐痰。淹没的后障绳泻湖通常排除海洋沙子供应到海东时间中期至晚期的沙丘片内部,尽管例外情况沿着一些海洋和泻湖海岸线发生。在沙丘片内部的后期更新世沙丘沉积物的重新激活导致一般薄(厚度为13米),但覆盖全新世沙丘沉积物(0.41 +/- 0.05至10.5 +/- 1.6 ka)。将需要机械钻孔来穿透封闭的底层Caliche层,以达到基础优质烯醇的Dune沉积物。 (c)2017 Elsevier B.v.保留所有权利。

著录项

相似文献

  • 外文文献
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