巴彦浩特
1.TECTONIC CHARACTERISTICS AND EVOLUTION OF BAYANHOT BASIN,WESTERN INNER MONGOLIA
2.Hydrocarbon-bearing prospect evaluation of Carboniferous from Hexi corridor to Bayan Haot basin
3.DISCOVERY OF PALEOZOIC SEDIMENTS IN EAST BAYANHOT BASIN AND ITS TECTONIC SIGNIFICANCE
4.Mixed Deep-Water Gravity Current Sedimentary Sequences of Middle-Ordovician Series in the East Margin of Bayanhaote Basin
5.Bayanhot basin has three depositional systems including lagoon-tidal flat, delta-fan delta and offshore shallow sea.
6.There are well source-reservoir-cap rock assemblages and suitable petroleum pool-forming conditions in Carboniferous strata.
7.The fractal dimension of aeromagnetic data from Bayanhaote basin was calculated and used for highlight and description of lithology.
8.Carboniferous strata, more than 1000m in thick in the area of Hexi corridor to Bayan Haot basin, is the coal measures of transitional phase, in which there are three kinds of hydrocarbon source rocks including dark mudstone, limestone, coal and carbonaceous mudstone.
9.The ecological environment planning and construction are important guarantee to realize the sustainable development of region and urban in arid areas. The research on Urban ecological environment planning in arid area was developed,taking the Ba Yan Hot of eastern edge of Teng Ge Li desert as an example.
10.The authors considered that the Bayanhaote Basin and its peripheral regions experienced the evolutionary stages of the Early Middle Proterozoic Qin Qi He Trigeminal Rift,the Late Proterozoic Cambrian Ordovician Aulacogen,the Silurian Devonian Foreland Basin,the Carboniferous Permian Compound Basin and the Mesozoic Cenozoic Fault Basin.
