Thermal history and basin evolution of the Moatize - Minjova Coal Basin (N'Condédzi sub-basin, Mozambique) constrained by organic maturation levels
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چکیده
منابع مشابه
Calculation of environmental water requirement in Great Karoun basin and upper Karoun sub-basin
The environmental requirement of the river is the amount of water to maintain natural ecological conditions and health of quality of the river water. In this study, to estimate the environmental water requirement of Karoun River, Dez, Great Karoun and Beheshtabad sub-basin (upper Karoun) using hydrological Montana method and offers based on frequency analysis of hydrological flow normally and u...
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The Alborz coal basin is located in northern part of Iran. The coal deposits of Shahrood in eastern Alborz, Zirab in central Alborz and Abyek in western Alborz were studied as typical coalfields of the basin. Shemshak Formation which is the main coal-bearing sequence was formed during the Triassic-Jurassic in the basin. It consists of sandstone, siltstone, shale and claystone, which variedly al...
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The Turkana Basin preserves a long and detailed record of biotic evolution, cultural development, and rift valley geology in its sedimentary strata. Before the formation of the modern basin, Cretaceous fluvial systems, Paleogene lakes, and Oligo-Miocene volcano-sedimentary sequences left fossil-bearing strata in the region. These deposits were in part related to an early system of rift basins t...
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a The Johns Hopkins University Applied Physics Laboratory, Laurel, MD 20723, USA Department of Terrestrial Magnetism, Carnegie Institution of Washington, Washington, DC 20015, USA Department of Geology, University of Georgia, Athens, GA 30602, USA Department of Earth, Environmental and Planetary Sciences, Brown University, Providence, RI 02912, USA e Planetary Geodynamics Laboratory, NASA Godda...
متن کاملGeodynamic history and sedimentary basin model of Hezardareh Formation
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ژورنال
عنوان ژورنال: Journal of African Earth Sciences
سال: 2019
ISSN: 1464-343X
DOI: 10.1016/j.jafrearsci.2019.02.020