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作 者:田涛[1] 任战利[1] 吴晓青[1] 马国福 张睿胜 杨智明 王维[3] 王锦[1]
机构地区:[1]西北大学大陆动力学国家重点实验室,陕西西安710069 [2]中国石油玉门油田分公司,甘肃酒泉735000 [3]中国石油长庆油田分公司,陕西西安710021
出 处:《中南大学学报(自然科学版)》2015年第8期2974-2982,共9页Journal of Central South University:Science and Technology
基 金:国家自然科学基金资助项目(41372128);西北大学大陆动力学国家重点实验室科技部专项经费资助项目(BJ08133-1)~~
摘 要:运用磷灰石裂变径迹(AFT)分析方法,探讨分析雅布赖盆地萨尔台凹陷中—新生代构造热事件发生的径迹年龄(AFTA)和长度(AFTL)分布特征,并通过反演法建立热史模型,恢复构造热演化过程。研究结果表明:研究区可能至少经历了3期隆升过程,分别发生在晚侏罗世末期((138.0±10)-135.8 Ma)、早白垩世晚期((116.0±8)-109.3Ma)和古近纪中晚期(52.0-29.4 Ma)。在时间演化上,新河组下段(J2x1)地层在盐场次凹和小湖子次凹具有相似性,但后者地层温度普遍高于前者,尤其在早白垩世,拥有更利于油气生成的地温环境。发生在180.0-146.7 Ma和130.5-100.0 Ma期间的2次增温过程与烃源岩热演化关系密切,地层温度可加热至72.0-135.0℃,是影响油气生成的关键阶段。构造热演化过程的研究为雅布赖盆地萨尔台凹陷的石油、天然气等矿产资源的勘探提供了新的约束条件。The characteristics of apatite fission track age(AFTA) and length(AFTL) data of the Meso-cenozoic tectonic-thermal history of Sartai depression of Yabrai basin were revealed by apatite fission track analysis. And the thermal history model was established by inversion method to recover the tectonic-thermal evolution. The results show that the study area may have experienced three times of uplift process at least which occurred in the end of Jurassic((138.0±10)-135.8 Ma), late stage of Early Cretaceous((116.0±8)-109.3 Ma) and middle-late Paleogene(52.0-29.4 Ma). The J2x1 strata in Yanchang sub-sag and Xiaohuzi sub-sag have the similar thermal evolution process in time, but the temperature of J2x1 in Xiaohuzi sub-sag is generally higher than that in Xiaohuzi sub-sag, especially in the Early Cretaceous when Xiaohuzi sub-sag had a much better geothermal field environment for hydrocarbon generation. The temperature of J2x1 heats up to 72.0-135.0 ℃ during 180.0-146.7 Ma and 130.5-100.0 Ma, and the two warming processes are the crucial stages of the source rock's maturity evolution and hydrocarbon generation in study area. The study of tectonic-thermal history can provide some new constraints on oil-gas and other mineral exploration in Yabrai Basin.
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