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Crustal Structure and Quaternary Acceleration of Deformation Rates in Central Washington Revealed by Stream Profile Inversion, Potential Field Geophysics, and Structural Geology of the Yakima Folds

机译：由亚基侧折叠的流型反转，潜在场地球物理和结构地质透露，华盛顿中心地壳结构和第四纪加速率

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Lydia Staisch; Richard Blakely; Harvey Kelsey; Richard Styron; Brian Sherrod;
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1. Crustal Structure and Quaternary Acceleration of Deformation Rates in Central Washington Revealed by Stream Profile Inversion, Potential Field Geophysics, and Structural Geology of the Yakima Folds [J] . Staisch Lydia, Blakely Richard, Kelsey Harvey, Tectonics . 2018,第5a6期

机译：流剖面反演，势场地球物理学和亚基马褶皱的构造地质揭示了华盛顿中部的地壳结构和第四纪形变速率
2. Deformation of Quaternary strata and its relationship to crustal folds and faults, south-central Puget Lowland, Washington State [J] . Derek B. Booth, Kathy Goetz Troost, Jonathan T. Hagstrum Geology . 2004,第6期

机译：华盛顿州中南部普吉低地第四纪地层的变形及其与地壳褶皱和断层的关系
3. Deformation of Quaternary strata and its relationship to crustal folds and faults, south-central Puget Lowland, Washington State [J] . Booth DB, Troost KG, Hagstrum JT Geology . 2004,第6期

机译：华盛顿州中南部普吉低地第四纪地层变形及其与地壳褶皱和断层的关系
4. Permeability potential modeling of geothermal prospects combining regional crustal strain rates with geomechanical simulation of fault slip and volcanic center deformation: A case study for Washington State geothermal play fairways [C] . Swyer M.W., Cladouhos T.T., Forson C., U.S. Symposium on Rock Mechanics . 2016

机译：地区地壳应变率与故障滑倒和火山中心变形地质力学模拟结合地热应变率的渗透性潜力建模 - 以华盛顿州地热播放球道为例
5. Upper crust structural and morphological ensembles of the Pamir-Tien Shan segment of Central Asia and their reflection in geophysical fields [O] . 2018

机译：中亚Pamir-Tien Shan Semment的上层地壳结构和形态集合及其在地球物理领域的反思
6. Structural Geometry, Strain Distribution, and Mechanical Evolution of Eastern Umtanum Ridge and a Comparison with Other Selected Localities within Yakima Fold Structures, South-Central Washington [R] . Price, E. H. 1982

机译：东部Umtanum岭的结构几何，应变分布和机械演化以及与亚基马褶皱构造中其他选定地点的比较，华盛顿中南部

Crustal Structure and Quaternary Acceleration of Deformation Rates in Central Washington Revealed by Stream Profile Inversion, Potential Field Geophysics, and Structural Geology of the Yakima Folds

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