Collaborative Research: Improved Cenozoic Plate Reconstructions of the Circum-Antarctic Region

合作研究：改进环南极地区新生代板块重建

• 批准号: 0126340
• 负责人: Steven Cande
• 金额: $ 16.66万
• 依托单位: University of California-San Diego Scripps Inst of Oceanography
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2002
• 资助国家: 美国
• 起止时间: 2002-04-15 至 2005-03-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0126340&HistoricalAwards=false
• 关键词: Collaborative; Research; Improved; Cenozoic; Plate

This award, provided by the Antarctic Geology and Geophysics Program of the Office of Polar Programs, provides funds for a project to make use of ship-repositioning transit cruises to gather geophysical information relating to plate tectonics of the Southern Ocean and to support student training activities. Well-constrained Cenozoic plate reconstructions of the circum-Antarctic region are critical for examining a number of problems of global geophysical importance. These problems include, e.g., relating the plate kinematics to its geological consequences in various plate circuits (Pacific-North America, Australia-Pacific); a dynamical understanding of what drives plate tectonics (which requires well-constrained kinematic information in order to distinguish between different geodynamic hypotheses); and an understanding of the rheology of the plates themselves, including the amount of internal deformation they can support, and the conditions leading to the formation of new plate boundaries through breakup of existing plates. By obtaining better constraints on the motion of the Antarctica plate with respect to these other plates, and by better quantifying the internal deformation within Antarctica (between East and West Antarctica), contributions will be made to solving these other fundamental problems.In this project, existing data will be analyzed to address several specific issues related to plate motions involving the Antarctic plate. First, work will be done on four-plate solutions of Australia-Pacific-West Antarctica-East Antarctica motion, in order to most tightly constrain the rotation parameters for separation between East and West Antarctica for the time period from about 45 to 28 Ma (Adare Basin spreading system). This will be done by imposing closure on the four-plate circuit and using relevant marine geophysical data from all four of the boundaries. The uncertainties in the resulting rotation parameters will be determined based on the uncertainties in the data points. These uncertainties can then be propagated in the plate circuit for use in addressing the various global geodynamic problems mentioned above. Second, rotation parameters for Pacific-West Antarctica during Tertiary time will be determined using recently acquired well-navigated Palmer transit data and any additional data that can be acquired during the course of this project. These parameters and their uncertainties will be used in assessments of plate rigidity and included in the plate circuit studies.In the framework of this project, new collection of marine geophysical data will be accomplished on a very flexible schedule. This will be done by collecting underway gravity, magnetics, and swath bathymetric data on Palmer transit cruises of geological importance. This has been successfully done on eight previous Palmer cruises since 1997, the most recent four of which were funded under a collaborative OPP grant to CalTech and Scripps which is now expiring. On one of the suitable transits, a formal class in marine geophysics will be conducted that will afford an opportunity to 12 or more graduate and undergraduate students, from CalTech and Scripps as well as other institutions. In this way, educational activities will be integrated with the usual scientific data collection objectives of the research project.

该奖项由极地项目办公室的南极地质和地球物理项目提供，为一个利用船舶重新定位过境巡航收集与南大洋板块构造有关的地球物理信息并支持学生培训活动的项目提供资金。约束良好的环南极地区新生代板块重建对于研究许多重要的全球地球物理问题至关重要。这些问题包括，例如，在各种板块回路（太平洋-北美，澳大利亚-太平洋）中，将板块运动学与其地质后果联系起来；对驱动板块构造的动力学理解（这需要良好约束的运动学信息，以便区分不同的地球动力学假设）；以及对板块本身流变学的理解，包括它们可以承受的内部变形量，以及通过现有板块的分裂导致新板块边界形成的条件。通过对南极洲板块相对于这些其他板块的运动获得更好的约束，并通过更好地量化南极洲内部（南极洲东部和西部之间）的变形，将有助于解决这些其他基本问题。在这个项目中，将分析现有数据，以解决与涉及南极板块的板块运动有关的几个具体问题。首先，将对澳大利亚-太平洋-南极洲西部-南极洲东部运动的四板块解进行研究，以最严格地约束约45 ~ 28 Ma （Adare盆地扩张系统）的东西南极洲分离的旋转参数。这将通过关闭四板块电路并使用来自所有四个边界的相关海洋地球物理数据来完成。结果旋转参数的不确定性将根据数据点的不确定性来确定。然后，这些不确定性可以在板块电路中传播，用于解决上述各种全球地球动力学问题。其次，太平洋-西南极洲第三纪期间的旋转参数将使用最近获得的导航良好的帕尔默过境数据和在该项目过程中可能获得的任何其他数据来确定。这些参数及其不确定性将用于板刚度的评估，并包括在板电路的研究中。在这个项目的框架内，新的海洋地球物理数据收集将在一个非常灵活的时间表上完成。这将通过收集帕尔默过境巡航的重力、磁力和带状水深数据来完成，这些数据具有地质重要性。自1997年以来，这已经成功地完成了8次帕尔默巡航，最近的4次是由加州理工学院和斯克里普斯的OPP合作资助的，该资助现已到期。在其中一个合适的凌日期间，将举办一次正式的海洋地球物理学课程，为来自加州理工学院和斯克里普斯以及其他机构的12名或更多的研究生和本科生提供机会。这样，教育活动将与研究项目通常的科学数据收集目标相结合。