共查询到20条相似文献，搜索用时 93 毫秒
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为探查容城地热田地热资源,中国地质调查局在雄安新区部署了地热勘探井D15井。D15井设计井深3000 m,完钻井深3111.58 m。钻探目的是为揭露容城凸起北部斜坡带地层发育情况,服务于新区地热开发规划。本文介绍了D15井的井区及地质状况、钻探施工情况;总结了取得的钻探成果,包括完成的钻探施工任务和施工质量;提炼出水热型地热井钻井液技术,优选取心工具,以及获取了岩心等实物资料;实施射孔作业完成了目的层抽水试验,获取的地层水温、水量等参数,为雄安新区地热资源调查评价提供了资料。 相似文献
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康定县地热资源丰富,但开发利用少,仅2008-2009年由四川省地质工程勘察院在中谷地区实施地热勘探井2口,钻探深度共计184.96m。DZK02井是部署在四川省雅拉河中上游热水塘区块地热资源大盖沟沟口雅拉河右岸一级阶地上的第一口预探井,设计井深2 000m。钻井施工主要面临地层倾角大、地层出水量大、温度高、岩性破碎等施工难题。施工队伍采用螺杆纠斜、清水控压等钻井工艺,圆满完成了该井的施工任务。为该地区地热水的开发利用进行了有益的尝试。 相似文献
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河南WR-1地热勘探井设计有新近系馆陶组和奥陶系2个勘探目的层,需要各自进行成井和测试工作,馆陶组成井测试完成后需要继续钻进完成奥陶系成井。在井身结构设计时,从套管设计、固井结构等方面进行优化改进,解决了馆陶组成井管柱固井、钻孔与套管级配以及过滤器参数设计等问题,并通过实钻验证。本文主要介绍了该地热勘探井井身结构设计过程中需要考虑的重点要素、设计过程等,并结合实钻过程,对井身结构的设计进行了调整和优化,使其更具现场操作性,为其它类似同井双目的层地热勘探井工程提供理论和实践参考。 相似文献
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为打赢大气污染防治攻坚战和燃煤替代任务,平顶山市市委市政府委托河南省有色金属地质矿产局组织开展平顶山地区地热勘查开发工作。根据对区域地质情况和地层特点,河南省有色金属地质矿产局自行设计并组织施工了平顶山北地热示范区PBR01井。文章从钻探设备选型、施工工艺选择、钻井液配置等方面介绍了项目设计和施工的全过程;通过钻井的施工,解决了本地区大口径深孔钻进难题,为本地区后续开发应用起到了良好的示范作用;通过对钻时曲线的分析,掌握了本地区不同地层钻进效率情况,提出了提高大直径硬岩钻进效率的方案。 相似文献
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西湖1井是准噶尔盆地南缘深部地层进一步油气勘探研究提供基础资料而部署的一口风险预探井。该井钻探构造高陡,钻遇断裂多,地层变化大,钻前地层压力预测更为重要。在地震地质解释研究的基础上,综合分析了工区内已钻的异常压力分布情况和形成机理,确定了本区地层压力的经验公式。通过对地震速度研究,建立三维速度场,进行层速度反演,提取井点地震速度。正确地估算了西湖1井的地层压力,为井身结构工程设计提供了依据,确保了钻井的顺利,地层压力预测结果与完钻后地层压力测试一致。 相似文献
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隆平1井是大庆油田首口在沉积盆地基底层施工的水平井，设计斜深4532.72 m（垂深3111.50 m），勘探钻井目的是为了探索通过水平井大幅度提高古中央隆起带基岩风化壳储层天然气产能。针对该井在钻井过程中可能遇到的难点与风险，进行了井身结构优化设计、井眼轨道优化设计、钻井参数优化、钻头优选及配套提速试验等。实钻情况表明，该井全井平均机械钻速5.15 m/h，相比设计钻速提高45.89%，现场施工提速效果明显，为探索该区域基底构造提供了宝贵的经验。 相似文献
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PBR01井是河南省有色金属地质矿产局在平顶山北组织实施的一口地热勘查示范井。完井深度2248.56 m,终孔直径216 mm。施工过程中遇到涌水、漏失、坍塌掉块、水敏失稳造浆等复杂地层及岩心采取率低等问题。本文从地层情况、井身结构设计、钻井工艺技术等方面介绍了该井的施工情况,总结取得的成果。通过采用改善钻井液性能、工艺堵漏、改进坚硬地层取心工艺、平衡法固井等措施解决施工中遇到的难题,为今后该地区中深部地热钻探积累一定的经验和技术。 相似文献
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Inter-regional correlation of transgressions and regressions in the Cretaceous period 总被引：1，自引：0，他引：1
T. Matsumoto 《Cretaceous Research》1980,1(4):359-373
Well investigated platforms have been selected in each continent, and the history of Cretaceous transgressions and regressions there is concisely reviewed from the available evidence. The factual records have been summarized into a diagram and the timing of the events correlated between distant as well as adjoining areas.On a global scale, major transgressions were stepwise enlarged in space and time from the Neocomian, via Aptian-Albian, to the Late Cretaceous, and the post-Cretaceous regression was very remarkable. Minor cycles of transgression-regression were not always synchronous between different areas. Some of them were, however, nearly synchronous between the areas facing the same ocean.Tectono-eustasy may have been the main cause of the phenomena of transgression-regression, but certain kinds of other tectonic movements which affected even the so-called stable platforms were also responsible for the phenomena. The combined effects of various causes may have been unusual in the Cretaceous, since it was a period of global tectonic activity. The slowing down of this activity followed by readjustments may have been the cause of the global regression at the end of the Cretaceous. 相似文献
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The Afyon stratovolcano exhibits lamprophyric rocks, emplaced as hydrovolcanic products, aphanitic lava flows and dyke intrusions, during the final stages of volcanic activity. Most of the Afyon volcanics belong to the silica-saturated alkaline suite, as potassic trachyandesites and trachytes, while the products of the latest activity are lamproitic lamprophyres (jumillite, orendite, verite, fitztroyite) and alkaline lamprophyres (campto-sannaite, sannaite, hyalo-monchiquite, analcime–monchiquite). Afyon lamprophyres exhibit LILE and Zr enrichments, related to mantle metasomatism. 相似文献
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正20140751 Guo Xincheng(Geological Party,BGMRED of Xinjiang,Changji 831100,China);Zheng Yuzhuang Determination and Geological Significance of the Mesoarchean Craton in Western Kunlun Mountains,Xinjiang,China(Geological Review,ISSN0371-5736,CN11-1952/P,59(3),2013,p.401-412,8 相似文献
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正20141058 Chen Ling(Key Laboratory of Mathematical Geology of Sichuan Province,Chengdu University of Technology,Chengdu610059,China);Guo Ke Study of Geochemical Ore-Forming Anomaly Identification Based on the Theory of Blind Source Separation(Geosci- 相似文献
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正20141334 Chen Kun(Institute of Geophysics,China Earthquake Administration,Beijing100081,China);Yu Yanxiang Shakemap of Peak Ground Acceleration with Bias Correction for the Lushan,Sichuan Earthquake on April20,2013(Seismology and Geology,ISSN0253-4967,CN11-2192/P,35(3),2013,p.627-633,2 illus.,1 table,9 refs.)Key words:great earthquakes,Sichuan Province 相似文献
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正20141624 Cai Xiongfei(Key Laboratory of Geobiology and Environmental Geology,Ministry of Education,China University of Geosciences,Wuhan 430074,China);Yang Jie A Restudy of the Upper Sinian Zhengmuguan and Tuerkeng Formations in the Helan Mountains(Journal of Stratigraphy,ISSN0253-4959CN32-1187/P,37(3),2013,p.377-386,5 illus.,2 tables,10 refs.) 相似文献
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正20142263Lü Shaojun(Geological Survey of Jiangxi Province,Nanchang 330030,China)Early-Middle Permian Biostratigraphical Characteristics in Qiangduo Area,Tibet(Resources SurveyEnvironment,ISSN1671-4814,CN32-1640/N,34(4),2013,p.221-227,2illus.,2tables,22refs.)Key words:biostratigraphy,Lower Permian,Middle Permian,Tibet 相似文献
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正20142560Hu Hongxia(Regional Geological and Mineral Resources Survey of Jilin Province,Changchun 130022,China);Dai Lixia Application of GIS Map Projection Transformation in Geological Work(Jilin Geology,ISSN1001-2427,CN22-1099/P,32(4),2013,p.160-163,4illus.,2refs.) 相似文献
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正20140692 Duo Tianhui(No.402 Geological Team,Exploration of Geology and Mineral Resources of Sichuan Authority,Chengdu611730,China);Wang Yongli Computer Simulation of Neptunium Existing Forms in the Groundwater(Computing Techniques for Geophysical and Geochemical Exploration,ISSN1001-1749,CN51-1242/P,35(3), 相似文献
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正20140876 Gao Junbo(College of Resources and Environmental Engineering,Guizhou University,Guiyang 550025,China);Yang Ruidong Study on the Strontium Isotopic Composition of Large Devonian Barite Deposits from Zhenning,Guizhou Province(Geochimica, 相似文献