Arid
来源IDNTRS_Document_ID: 19940026603
State of stress, faulting, and eruption characteristics of large volcanoes on Mars
Mcgovern, Patrick J.; Solomon, Sean C.
英文摘要The formation of a large volcano loads the underlying lithospheric plate and can lead to lithospheric flexure and faulting. In turn, lithospheric stresses affect the stress field beneath and within the volcanic edifice and can influence magma transport. Modeling the interaction of these processes is crucial to an understanding of the history of eruption characteristics and tectonic deformation of large volcanoes. We develop models of time-dependent stress and deformation of the Tharsis volcanoes on Mars. A finite element code is used that simulates viscoelastic flow in the mantle and elastic plate flexural behavior. We calculate stresses and displacements due to a volcano-shaped load emplaced on an elastic plate. Models variously incorporate growth of the volcanic load with time and a detachment between volcano and lithosphere. The models illustrate the manner in which time-dependent stresses induced by lithospheric plate flexure beneath the volcanic load may affect eruption histories, and the derived stress fields can be related to tectonic features on and surrounding martian volcanoes.
英文关键词ELASTIC PLATES FINITE ELEMENT METHOD GEOLOGICAL FAULTS LITHOSPHERE MARS SURFACE MARS VOLCANOES PLANETARY GEOLOGY STRESS ANALYSIS STRESS DISTRIBUTION TECTONICS VISCOELASTICITY VOLCANOES VOLCANOLOGY DEFORMATION LOADS (FORCES) MAGMA
出版年1993
报告类型Technical Report
语种英语
国家美国
URLhttp://hdl.handle.net/2060/19940026603
资源类型科技报告
条目标识符http://119.78.100.177/qdio/handle/2XILL650/259206
推荐引用方式
GB/T 7714
Mcgovern, Patrick J.,Solomon, Sean C.. State of stress, faulting, and eruption characteristics of large volcanoes on Mars,1993.
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