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Articles 3841 - 3870 of 29940
Full-Text Articles in Geology
Mgrre_Thinsections_Mgrre-67_65, Mgrre
Mgrre_Thinsections_Mgrre-67_66, Mgrre
Mgrre_Thinsections_Mgrre-67_74, Mgrre
Mgrre_Thinsections_Mgrre-67_76, Mgrre
Mgrre_Thinsections_Mgrre-67_73, Mgrre
Mgrre_Thinsections_Mgrre-67_82, Mgrre
Mgrre_Thinsections_Mgrre-67_84, Mgrre
Mgrre_Thinsections_Mgrre-67_90, Mgrre
Mgrre_Thinsections_Mgrre-67_79, Mgrre
Mgrre_Thinsections_Mgrre-67_98, Mgrre
Mgrre_Thinsections_Mgrre-67_99, Mgrre
Mgrre_Thinsections_Mgrre-67_89, Mgrre
Mgrre_Thinsections_Mgrre-67_91, Mgrre
Mgrre_Thinsections_Mgrre-67_92, Mgrre
Mgrre_Thinsections_Mgrre-53_87, Mgrre
Induced Seismicity In The Raton Basin And Global Variability Of The 410-Km Discontinuity, Margaret E. Glasgow
Induced Seismicity In The Raton Basin And Global Variability Of The 410-Km Discontinuity, Margaret E. Glasgow
Earth and Planetary Sciences ETDs
Natural processes like mantle convection and plate tectonics dominate Earth’s seismic structure. Recently human activities have increasingly influenced the deformation of the shallow crust. In this dissertation, passive source seismology was used to constrain seismic discontinuities in the mantle transition zone and seismogenic structures in induced earthquake settings. Using a novel sampling method and uniform processing approach, I found the 410-km discontinuity is thermally and compositionally variable. Using a machine- learning approach, I found the three main zones of seismicity in the Raton Basin consist of short faults or fault segments with variable orientations. The zone that hosted a Mw …
Mgrre_Thinsections_Mgrre-67_40, Mgrre
Mgrre_Thinsections_Mgrre-46_8, Mgrre
Mgrre_Thinsections_Mgrre-53_14, Mgrre
Mgrre_Thinsections_Mgrre-41_11, Mgrre
Mgrre_Thinsections_Mgrre-40_21, Mgrre
Mgrre_Thinsections_Mgrre-43_7, Mgrre
Mgrre_Thinsections_Mgrre-44_6, Mgrre
Mgrre_Thinsections_Mgrre-46_1, Mgrre
Mgrre_Thinsections_Mgrre-46_52, Mgrre
Mgrre_Thinsections_Mgrre-46_60, Mgrre
Mgrre_Thinsections_Mgrre-46_83, Mgrre
Mgrre_Thinsections_Mgrre-46_85, Mgrre