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61.
塔中地区奥陶系埋藏热液溶蚀流体活动及其对深部储层的改造作用 总被引:2,自引:0,他引:2
基于矿物流体包裹体均一化温度、热液矿物分布及其地球化学特征等,识别出了塔中地区重点研究井段埋藏热液溶蚀流体化学性质,探讨其在纵横向的分布及流动特征。研究表明,(1)埋藏热液溶蚀流体在塔中地区较为活跃,并对碳酸盐岩储层有着良好的改造效应,油气勘探前景广阔;(2)北东-南西向走滑断裂发育地带有利于埋藏热液溶蚀流体的注入,研究区TZ45以及TZ82-TZ16井区均是埋藏热液溶蚀流体异常活跃地带。同时,研究还认为,早期表生岩溶作用产生的溶洞体系将被后期埋藏压实作用部分破坏,而其残余空间往往是埋藏热液溶蚀流体进入储层的优势通道,继而发生溶蚀改造扩大溶洞空间。因此,在塔里木深部碳酸盐岩储层的勘探过程中,应充分重视挤压背景下张性断裂的发育及其热流体疏导效应,如走滑断裂强烈活动地带;同时应着重注意多期不同性质流体的叠加改造效应,这些区域可作为优选勘探目标。 相似文献
62.
The first exploratory well, the ZS1C well, with 158,545 m3 daily gas production was discovered in 6861–6944 m deep strata of the Cambrian gypsolyte layer of the Tarim Basin, China in 2014. The discovery opens a new target for the Cambrian-reservoired oil and gas exploration, and directly leads to large-scale oil and gas exploration of the deep-reservoired Cambrian oil and gas fields in the Basin. Comprehensive two-dimensional gas chromatography/time-of-flight mass spectrometry and a comprehensive two-dimensional gas chromatography–flame ionization detector revealed the presence of abundant adamantane compounds, 2-thiaadamantanes and 2-thiadiamantanes, and a large amount of sulfur-containing compounds in the condensate oil. The formation of organic sulfur-containing compounds, such as 2-thiaadamantanes, is an indication of sulfur incorporation from the gypsum in the stratum into oil and gas in the course of TSR. This reservoir has apparently suffered severe TSR alteration because (1) High content of H2S, (2) H2S sulfur isotopes, (3) CO2 carbon isotopes, and others abundant data to support this findings. Similar sulfur isotopic composition of H2S, oil condensate and the gypsum in the Cambrian strata indicate that the produced condensate is experienced TSR alteration. Therefore, the deep-accumulated Cambrian oil reservoir has experienced severe TSR alteration, and accumulated natural gas and condensate contains high sulfur content. 相似文献
63.
正Evaporite series is both an important target area looking for high-quality large potash deposits,but also one of the main types of hydrocarbon cap.Outcrops and drilling results indicate that five sets of evaporites were developed 相似文献
64.
塔里木盆地塔中I号断裂带西缘奥陶系油气成藏与主控因素研究 总被引:3,自引:0,他引:3
塔中低凸起是塔里木盆地油气资源最丰富的地区之一,而塔中I号断裂带西缘也在多个层系中见到了不同程度的油气显示,并在上奥陶统良里塔格组获得了高产工业油气流,在下奥陶统鹰山组获得了低产油气流.本文通过油源对比、油气水物性对比、包裹体均一温度分析等方法并结合前人的研究成果,探讨了塔中I号断裂带西缘塔中86井区-塔中45井区奥陶系的油气成藏过程,认为该区奥陶系有过三期油气充注,即晚加里东期、晚海西期和燕山期-喜马拉雅期.晚加里东期的油气来自于寒武系-下奥陶统烃源岩,晚海西期的油气来自于中-上奥陶统烃源岩,两期油气均自塔中88井沿碳酸盐岩岩溶储层侧向运移而来;燕山期-喜马拉雅期主要以天然气为主,成因复杂.另外,认为该区油气富集的主控因素主要有3点:多源多期油气充注、优质的碳酸盐岩岩溶储层及各种成藏要素的优质配置. 相似文献