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Diatom Biostratigraphy & Paleoceanography of the Santa Cruz Mudstone

Diatom Biostratigraphy & Paleoceanography of the Santa Cruz Mudstone
硅藻生物地层学
批准号:
9212565
负责人:
Lisa White
金额:
$1.2万
依托单位国家:
美国
项目类别:
Standard Grant
财政年份:
1992
资助国家:
美国
项目状态:
已结题
起止时间:
1992-09-01 至 1994-02-28

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中文摘要
翻译
圣克鲁斯泥岩是加利福尼亚州中北部的一个厚的硅质泥岩单元(约2000米),似乎与中新世蒙特利组的上部相关。该单元暴露在Bolinas-Point Reyes和Santa Cruz地区,在这些地区,它已被圣安德烈亚斯断层系统的运动显著抵消。圣克鲁斯泥岩的年代、地层和古海洋学鲜为人知。对圣克鲁斯泥岩进行多年研究的主要目标将是:(1)利用硅藻生物地层学精确测定圣克鲁斯泥岩的年龄;(2)描述和记录富硅和富碳酸盐岩石之间的地层旋回;(3)评估圣克鲁斯泥岩内突出的层理旋回和其他地层变化的时间和古海洋学意义。规划期将有助于初步数据收集和多年期研究计划的有效评估。规划年的两个主要目标是:(1)进行实地勘察工作和采样(硅藻)和(2)评估和综合实地和年龄数据,并撰写一份具有竞争力的多年研究计划。这项调查最重要的方面是,预计调查结果将反映中新世晚期复杂的气候和海平面变化。这样的结果将增加我们对古代上升流、高肥力系统下沉积的沉积物的理解。
英文摘要
The Santa Cruz Mudstone is a thick unit (approximately 2000m) of siliceous mudstones in north-central California that appears to be correlative with the upper part of the Miocene Monterey Formation. The unit is exposed in the Bolinas-Point Reyes and Santa Cruz areas where it has been significantly offset by movement along the San Andreas fault system. The age, stratigraphy, and paleoceanography of the Santa Cruz Mudstones are poorly known. The major objectives of a multi-year study on the Santa Cruz Mudstone would be: (1) to precisely date the age of the Santa Cruz Mudstone using diatom biostratigraphy, (2) to describe and document stratigraphic cycles between silica-rich and carbonate-rich rocks, and (3) to assess the timing and paleoceanographic significance of prominent bedding cycles and other stratigraphic variations within the Santa Cruz Mudstone. A planning period will facilitate preliminary data collection and the effective evaluation of a multi-year research plan. Two major objectives during the planning year are: (1) to conduct reconnaissance field work and sampling (for diatoms) and (2) evaluate and synthesize field and age data and write a competitive multi-year research proposal. The most significant aspect of this investigation is the results are expected to reflect complex climate and sea level variations during the late Miocene. Results such as these will increase our understanding of sediments deposited beneath ancient upwelling, high fertility systems.
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