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首页> 外文期刊>GSA Bulletin >Hydraulic piston coring of late Neogene and Quaternary sections in the Caribbean and equatorial Pacific: Preliminary results of Deep Sea Drilling Project Leg 68
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Hydraulic piston coring of late Neogene and Quaternary sections in the Caribbean and equatorial Pacific: Preliminary results of Deep Sea Drilling Project Leg 68

机译:加勒比海和赤道太平洋新近纪晚期和第四纪后期的液压活塞取芯:深海钻探项目第68腿初步结果

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摘要

Leg 68 of the Deep Sea Drilling Project used the newly developed Hydraulic Piston Corer (HPC) to recover two virtually continuous, undisturbed sections of late Neogene and Quaternary sediment. The sites are located in the western Caribbean (Site 502, 4 holes) and in the eastern equatorial Pacific (Site 503, 2 holes). The sediment of Site 502 is primarily foram-bearing nanno marl which accumulated at about 3 to 4 cm/thousand yr. The bottom of Site 502 (228.7 m) is 8 m.y. old. The sediment of Site 503 is primarily siliceous calcareous ooze which accumulated at about 2 to 3 cm/thousand yr. The bottom of Site 503 (235.0 m) is 8 m.y. old. The magnetostratigraphy of both sites was determined on the R.V. Glomar Challenger with a long-core spinner magnetometer. All paleomagnetic boundaries through the Gilbert were identified in Site 502; most of them were identified in Site 503. The sediment at both sites shows a distinct cyclicity of calcium carbonate content. These relatively high accumulation rate, continuous, undisturbed HPC cores will enable a wide variety of high-resolution biostratigraphic, paleoclimatic, and paleoceanographic studies heretofore not feasible.
机译:深海钻探项目的第68条腿使用新开发的 液压活塞Corer(HPC)回收了新近纪晚期和第四纪沉积物的两个几乎连续的 未扰动部分。 这些站点位于加勒比西部(Site 502,4 孔)和赤道东太平洋(Site 503,2孔)。 站点502主要是带有孔的Nanno marl ,其堆积速率约为3-4 cm /千年。站点502(228.7 m)的底部 为y 8 y。旧。站点503 的沉积物主要是硅质钙质软泥,堆积在 约2至3 cm /千年。 Site 503(235.0 m) 的底部是y.m.y. R.V。上确定了两个位置的磁地层学。 通过吉尔伯特(Gilbert)的所有古磁界都在站点502中被识别出 。它们中的大多数在站点503中被识别。两个站点的沉积物 都显示出明显的碳酸钙 含量周期性。这些相对较高的累积速率,连续的, 不受干扰的HPC岩心将能够进行各种高分辨率的 生物地层学,古气候学和古海洋学研究 可行。

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  • 来源
    《GSA Bulletin 》 |1980年第7期| 433-444| 共12页
  • 作者单位

    Department of Geological Sciences, Brown University, Providence, Rhode Island 02912;

    Pacific-Arctic Branch of Marine Geology, U.S. Geological Survey, 345 Middlefield Road, Menlo Park, California 94025;

    Deep Sea Drilling Project, Scripps Institution of Oceanography, La Jolla, California 92093;

    Lamont-Doherty Geological Observatory, Columbia University, Palisades, New York 10964;

    Department of Earth Sciences, Open University, Buckinghamshire, England;

    Graduate School of Oceanography, University of Rhode Island, Kingston, Rhode Island 02881;

    Lamont-Doherty Geological Observatory, Columbia University, Palisades, New York 10964;

    Department of Geology, University of Georgia, Athens, Georgia 30602;

    Institut für Sedimentforschung, Universitat Heidelberg, Im Neuenheimer Feld 236, Postfach 102020, D-6900, Heidelberg I, Federal Republic of Germany;

    School of Oceanography, University of Rhode Island, Kingston, Rhode Island 02881;

    Geological Research Division, Scripps Institution of Oceanography, La Jolla, California 92093;

    Lamont-Doherty Geological Observatory, Columbia University, Palisades, New York 10964;

    Lamont-Doherty Geological Observatory, Columbia University, Palisades, New York 10964;

    Department of Geology, Union College, Schenectady, New York 12308;

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