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哈得逊隆起是新近在塔里木盆地满加尔凹陷西部发现的一个向西南抬升、向北东方向倾伏的大型宽缓鼻状隆起 ,隆起构造主要发育在石炭系以上层位 ,以石炭系较为典型。构造演化史分析表明 ,哈得逊地区在前侏罗纪属于轮南古隆起的一部分 ,二者统一为一向西南倾伏、向北东抬升的大型古隆起构造 ,与现今哈得逊隆起的倾伏方向恰好相反。三叠纪末印支运动后 ,南抬北倾的哈得逊隆起开始形成。晚第三纪以来 ,满西地区石炭系地层也由区域南倾反转为区域北倾 ,并形成石炭系鼻状隆起。在石炭系地层发生翘式反转的过程中 ,哈得逊地区因正好处于翘倾运动的“支点”位置 ,构造位置适中 ,构造作用也相对比较稳定 ,因而对于油气聚集和保存十分有利 ,是满西地区寻找大中型油田最有利的地区。
The Hudson uplift is a large, broad nose-like uplift recently discovered in the west of Manjar sag in the Tarim Basin, which is uplifted to the southwest and plunges to the northeast. The uplift structure is mainly developed above the Carboniferous, with typical Carboniferous . Tectonic evolution history shows that the Hudson region was part of the Lunnan paleo-uplift in the Pre-Jurassic period, and the two are unified as a large paleohigh-uplift that has plunged to the southwest and uplifted to the northeast. Compared with the present Hudson uplift The opposite direction of the volt. After the Indosinian movement in the end of the Triassic, the Hudson uplift with a northward levee started to form. Since the Late Tertiary, the Carboniferous strata in Manxi area have also been inverted from south to south by region, forming a Carboniferous nasal uplift. During the reversal of warp type in the Carboniferous strata, the Hudson region is located at the “fulcrum” position of the tilting movement and has moderate tectonic position and relatively stable tectonic activity. Therefore, it is very favorable for the accumulation and preservation of hydrocarbons Manxi region to find the most profitable area of large and medium-sized oil fields.