Results 181 to 190 of about 151,860 (247)
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Accompanying Mud Volcanic Structures
2020This chapter describes the structures associated with mud volcanoes. Mud volcanic activity is accompanied by the eruption of huge volumes of gases, mud breccia, detrital rock material, and water. This has led to the creation of weakened zones in the depths near mud volcanoes due to the removal of sedimentary material.
Evgeny Shnyukov, Valentina Yanko-Hombach
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Origin of mud volcanism and diapirism
International Geology Review, 1983(1983). Origin of mud volcanism and diapirism. International Geology Review: Vol. 25, No. 8, pp. 877-881.
N. Vu. Khalilov, A. A. Kerimov
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Igneous or Mud Volcanism on Mars? The Case Study of Hephaestus Fossae
Journal of Geophysical Research: Planets, 2020Hephaestus Fossae are a system of northwest trending troughs west of the Elysium Mons volcanic construct on Mars. Pitted cones present in the fossae region have previously been interpreted as both igneous and mud volcanism products based on morphometry ...
A. Dapremont, J. Wray
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Fluid-dynamic modeling of mud volcanism
Russian Geology and Geophysics, 2011Abstract The eruptive behavior of mud volcanoes has been explored in several forward and inversion models. The forward models, based on classical continuum-mechanics, simulate the non-stationary processes of gas seepage and two-phase gas-mud flow through the conduit of a mud volcano, as well as the quasi-stationary gas frontal drive that
A.V. Domanskii, V.V. Ershov
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Carbonate mounds formed by mud volcanism at the Cretaceous-Paleogene boundary, Saudi Arabia
InterpretationMore than 1,000 mound structures have been mapped in shallow marine sediments at the Cretaceous Paleogene boundary in the Rub Al-Khali of Saudi Arabia. Mapping utilized 3D reflection seismic data in a 37,000 square kilometer study area.
S. A. Stewart, A. Muslem
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AIP Conference Proceedings, 2006
Mud volcanoes of Azerbaijan and the South‐Caspian Basin (SCB) are closely related to the tectonic processes in the basin and the orogenic system of the Greater and Lesser Caucasus. The maximum density of the mud volcanoes in Azerbaijan and the SCB is observed in the Shamakha‐Gobustan zone.
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Mud volcanoes of Azerbaijan and the South‐Caspian Basin (SCB) are closely related to the tectonic processes in the basin and the orogenic system of the Greater and Lesser Caucasus. The maximum density of the mud volcanoes in Azerbaijan and the SCB is observed in the Shamakha‐Gobustan zone.
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Some questions of the connection between mud volcanism and seismicity in Azerbaijan
Azerbaijan Oil IndustryThe article discusses some issues of the genetic connection between mud volcanic activity in Azerbaijan and seismicity, the results of monitoring studies of mud volcanoes characterized by active gryphon-salsa activity between eruptions located in ...
E. Baloglanov
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Modelling of possible mud volcanism on Titan
Icarus, 2006Possible sedimentary basins on Titan are potential sites for the formation of mud volcanoes. In order to constrain the appearance of such features in remotely sensed imagery being acquired by the Cassini spacecraft, we have modelled the formation of mud volcanoes on Titan for a series of plausible mud compositions, climatic conditions and geological ...
A. Dominic Fortes, Peter M. Grindrod
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Geochemical Patterns of Mud Volcanic Waters: Reviewed Worldwide Data
Geochemistry International, 2021This paper is the world’s first to generalize and analyze worldwide data on the chemical composition of waters from 175 onshore mud volcanoes. Empirical probability density functions are obtained for the dominant anions and cations, whose average concentrations (Clarke values) were also estimated.
O. A. Nikitenko, V. V. Ershov
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GEODYNAMICS
The purpose of the research was to substantiate the scientific basis behind the formation of a mud volcano within a specific section of the Precarpathian depression.
E. Kuzmenko +6 more
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The purpose of the research was to substantiate the scientific basis behind the formation of a mud volcano within a specific section of the Precarpathian depression.
E. Kuzmenko +6 more
semanticscholar +1 more source

