Houseknecht D W.Evolution from passive margin to foreland basin : the Atoka formation of the Arkoma Basin , south2central USA. Foreland Basins . 1986Evolution from passive margin to foreland basin, the Atoka formation of the Arkoma - Houseknecht - 1986...
a, Model A: the Great Indian continent model55where the long-term large-scale erosion of the passive margin produced large amounts of sediments whose subduction led to the acceleration of India–Eurasia convergence at 65 Ma.b, Model B: the Great Indian Basin model14,55; same as in model...
The evolution of a passive margin into a foreland basin has important implications for thepetroleum system. In Eastern Venezuela, for example, the subsidence caused by thrust/fold loading has taken the otherwise immature Guyana passive margin sequence into the petroleum window (Summa et al., 2003)...
a, Model A: the Great Indian continent model55where the long-term large-scale erosion of the passive margin produced large amounts of sediments whose subduction led to the acceleration of India–Eurasia convergence at 65 Ma.b, Model B: the Great Indian Basin model14,55; same as in model...
5) passive margin 被动边缘 1. In the Triassic, the sedimentary structural zones developed from passive margin basin to active margin basin as a result of the influence of the Jinshajiang suture zone and Garz Litang suture zone,and split apart into the Baiyu Yidun foreland basin,Chomta ...
South America is outlined. It is seen that an as-yet unknown Jurassic marine shelf section probably exists beneath northern Maturin Basin/Serranía del Interior/Trinidad which is correlative and probably similar to the western Cuban Jurassic stratigraphie section (initial conjugate rift margin). From ...
5) passive margin 被动边缘 1. In the Triassic, the sedimentary structural zones developed from passive margin basin to active margin basin as a result of the influence of the Jinshajiang suture zone and Garz Litang suture zone,and split apart into the Baiyu Yidun foreland basin,Chomta ...
Mesoproterozoic continent Passive margin Carbonate platform Brasiliano oceans Zircon U-Pb dating 1. Introduction The Stenian-Tonian Lajeado Group in the Ribeira Belt, southeastern Brazil (Fig. 1), corresponds to an open-sea carbonate platform and passive margin intruded in its upper portion by the ...
By Middle Trias a integrated Dian-Qian-Gui deep basin had been formed. 2.Packs belts in northern margin of Middle Triassic Dian-Qian-Gui deep basin Based on the rock texture , sedimentary structure and biological assemblages there are some facies belts (from north to south) as following: l....
5) passive margin 被动边缘 1. In the Triassic, the sedimentary structural zones developed frompassive marginbasin to active margin basin as a result of the influence of the Jinshajiang suture zone and Garz Litang suture zone,and split apart into the Baiyu Yidun foreland basin,Chomta Xiangcheng...