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Relative and absolute plate motion changes in the southeast Pacific: Cause and effect.

机译:东南太平洋板块相对运动和绝对运动的变化:因果关系。

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摘要

The purpose of this work is to expand upon our understanding of the dynamics of absolute plate motions and the interactions between plates using geological, geophysical, and modeling techniques.; Using fracture zone morphology and magnetics the following relationships are hypothesized: the Pacific-Farallon ridge reorganization began around 35 Ma, the reorganization took around 10 m.y., the greatest changes in ridge geometry took place adjacent to the Nazca portion of the Farallon plate, the Nazca plate underwent an absolute motion change around 26 Ma (O'Connor et al., 1996), South America was the only other plate in the region to under a change in absolute motion at this time (35 Ma), and thus the timing indicates that South America is the cause of Nazca's motion change. Two- and three-dimensional finite element models of the region establish that it is viable that the westward acceleration of South America could have transmitted a compressional stress to the Nazca portion of the Farallon plate, and that the east-west compressional stress generated by South America was transmitted to the ridge where it was concentrated across the transforms. The misalignment of the east-west compressional stress with the slip along the transforms may have impeded spreading and thus caused the ridge to reorganize. Shear stress in the slab at the northern boundary of South America due to South America's acceleration may also be related to the creation of a tear in the Pacific-Farallon slab at 30 Ma and the subsequent change in the absolute motion of the Nazca portion of the Farallon plate. These results lead to the conclusion that the westward acceleration of South America changed the force-balance of the Nazca portion of the Farallon plate, ulimately resulting in the reorganization of the Pacific-Farallon ridge and the 26 Ma absolute motion change of the Nazca plate.; This work was augmented by finite element studies of anomalous normal faulting earthquakes along the present day Eltanin transform system.
机译:这项工作的目的是扩展我们对绝对板块运动的动力学以及使用地质,地球物理和建模技术的板块之间相互作用的理解。使用断裂带的形态学和磁学,可以推测以下关系:太平洋-法拉隆脊重组发生在35 Ma左右,重组发生了约10 my,脊几何的最大变化发生在法拉隆板块的纳斯卡部分附近,纳斯卡板块在26 Ma左右经历了绝对运动变化( O'Connor等人,,1996),南美是该地区唯一在该时刻发生了绝对运动变化的其他板块(35 Ma ),因此时间表明南美洲是纳斯卡运动变化的原因。该区域的二维和三维有限元模型确定,南美洲的向西加速度可能已经向Faralon板块的纳斯卡部分传递了压应力,并且由南向产生的东西向压应力是可行的。美国被传播到山脊,在那里它集中了整个转变。东西向压缩应力与沿转换的滑移的不对齐可能已经阻碍了扩展,从而导致山脊重组。由于南美的加速,南美洲北部边界板上的剪应力也可能与太平洋地区的法拉隆板在30 Ma处产生裂缝以及随后纳斯卡部分纳斯卡部分的绝对运动发生变化有关。法拉隆板。这些结果得出的结论是,南美的向西加速改变了Farallon板块的纳斯卡部分的力平衡,最终导致太平洋—Farallon脊的重组和纳斯卡板块的26 Ma绝对运动变化。 ;这项工作通过沿现今Eltanin变换系统对异常正断层地震的有限元研究得到了加强。

著录项

  • 作者

    Beutel, Erin Kelly.;

  • 作者单位

    Northwestern University.;

  • 授予单位 Northwestern University.;
  • 学科 Geology.; Geophysics.
  • 学位 Ph.D.
  • 年度 2000
  • 页码 341 p.
  • 总页数 341
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 地质学;地球物理学;
  • 关键词

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