Palaeofluid evolution process in Well Block Tubei 1 in the Kuqa Depression, Tarim Basin

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• 作者：Hai Wu^a ; ^b ; Mengjun Zhao^a ; ^b ; ^{zmj@petrochina.com.cn" class="auth_mail" title="E-mail the corresponding author} ; Qingong Zhuo^a ; ^b ; Xuesong Lu^a ; ^b ; Weiqiang Li^c ; Fang Zeng^d ; Aiwen Zhao^c
• 关键词：Tarim Basin ; Kuqa Depression ; Northern Tuzimazha (Tubei) ; Fluid inclusion ; Quantitative grain fluorescence (QGF) ; Paleofluid evolution ; Total Scanning Fluorescene (TSF) ; Gypsum-salt rock ; Caprocks ; Natural gas ; Light oil
• 刊名：Natural Gas Industry B
• 出版年：2016
• 出版时间：March 2016
• 年：2016
• 卷：3
• 期：2
• 页码：129-138
• 全文大小：4254 K

文摘

Under the joint action of gypsum-salt rocks and faults, fluid evolution process is complicated in the northern Tuzimazha, Kuqa Depression, Tarim Basin. In the past, however, the oil and gas distribution rules in this area were less studied, so the related understanding was insufficient. In this paper, the reservoirs in Well Block Tubei 1 were analyzed by means of fluid inclusion and quantitative grain fluorescence (QGF) techniques. Based on tectonic evolution history, burial history, thermal history and hydrocarbon generation history, the paleofluid evolution process in this area was reproduced. It is shown that the well block experienced hydrocarbon charge in two periods. The first period is the early–middle stage (16–9 Ma) of Miocene Kangcun Fm (N_1–2k), when it was charged with oil, with the corresponding characteristics of yellow and white–yellow fluid inclusion fluorescence and the QGF Index higher than 4, indicating that there were paleo-oil reservoirs at the early stage of the reservoirs. And at the late stage, the fluids that were accumulated at the early stage escaped because the gypsum-salt rocks were cut by faults, and bitumen remained in the reservoirs. It is also the evidence for the escaping of the early charged oil that the total scanning fluorescence (TSF) of the hydrocarbon adsorbed to the surface of the current reservoirs is generally unimodal. The second period is the late stage (about 3 Ma) of Pliocene Kuqa Fm (N₂k), when the natural gas and light oil charging occurred. Correspondingly, there are two inclusions, i.e. black gaseous hydrocarbon inclusion and blue fluorescence inclusion located along the edge of the quartz grains. At this stage, the gypsum-salt caprocks deepened and their sealing capacity was recovered due to a strong plastic flow. Moreover, the trap was uplifted violently under the effect of Himalaya orogeny, and a large amount of natural gas and a little light oil were accumulated.