Episodic Accretion on the Mid-Atlantic Ridge: Interpretation and Sampling of Crustal Sections from the Kane Transform Fault
Episodic Accretion on the Mid-Atlantic Ridge: Interpretation and Sampling of Crustal Sections from the Kane Transform Fault
批准号:
8919244
负责人:
John Delaney
金额:
$43.25万
依托单位:
依托单位国家:
美国
项目类别:
Standard Grant
财政年份:
1990
资助国家:
美国
项目状态:
已结题
起止时间:
1990-07-01 至 1993-06-30
中文摘要
了解洋壳的组成和化学成分一直是海洋地球科学的长期目标。这些信息对将地幔物质转移到地壳的过程提供了重要的制约,这些过程导致火成岩地壳的形成,并随后改变地壳的化学成分和控制海水的成分。然而,这样的理解需要一种对地壳岩石进行取样的手段,以及一种将个别地壳层与上、下层联系起来的方法。尽管深部地壳钻探是一种这样的技术,但深部地壳洞穴成本很高,提供的地壳物质面积样本有限。最近,人们对研究断裂的地壳暴露重新产生了兴趣,将其作为一种通过潜水/挖泥或一系列浅钻孔对地壳岩石的地层序列进行取样的方法。本奖项将对北大西洋凯恩转换断层裸露的地壳岩石进行侧扫声纳调查。该项目的目标是绘制地壳各层的连续性图,对沿转换暴露的火成岩的地层序列进行采样,并检查沿主要陡坎暴露的断层模式。这些数据将被用来确定地壳增长的历史和随后的变形。此外,这些数据将为该地区随后的潜水研究提供所需的调查。该项目是华盛顿大学、杜克大学和巴黎大学的科学家合作研究。
英文摘要
Understanding the composition and chemistry of the oceanic crust has been a long term goal of the marine geosciences. Such information provides important constraints on the processes that transfer mantle material to the crust, that lead to the formation of the igneous crust, and that subsequently modify the chemistry of the crust and control the composition of seawater. Such an understanding, however, requires a means to sample crustal rock and a way to relate individual crustal layers to over- and underlying strata. Although deep crustal drilling is one such technique, deep crustal holes are expensive and provide limited areal sampling of crustal material. Recently there has been renewed interest in studying faulted crustal exposures as a way to sample a stratigraphic succession of crustal rocks by submersible/dredging or by a series of shallow drill holes. The present award will undertake a side-scan sonar survey of exposed crustal rocks in the Kane Transform Fault in the north Atlantic. Objectives of the project are to map the continuity of crustal layers, to sample the stratigraphic succession of igneous rocks exposed along the transform, and to examine the faulting pattern exposed along major scarps. These data will be used to determine both the history of crustal accretion and subsequent deformation. Additionally, these data will provide the needed survey for subsequent submersible research in the area. The project is a cooperative study between scientists at the University of Washington, Duke University and the University of Paris.
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会议论文
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Collaborative Research: Integrated Geological Interpretationof Deep-Tow Sonar, Submersible, and Petrological Observations of the Upper and Lower Oceanic Crust
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A Proposal to Support the 1992 RIDGE Theoretical Institute
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Constraints on Magma Chamber-Hydrothermal Interaction from the Seamail Ophiolite (Oman)
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国内基金
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依托单位: