褶皱变形区正负向构造单元页岩气差异富集特征     

张梦琳  李郭琴  寇一龙  李柯  陈佳  徐剑良  何嘉  梁霄  樊骐铖 《地质论评》2024,70(S1):272-274

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新疆塔里木盆地哈拉奇地区晚石炭世—早二叠世哈拉奇组的建立简   总被引：1，自引：0，他引：1  

张新勇  刘晓煌  李保飞  张雄华  刘龙龙  牛树银  寇晓虎  杨宝忠 《地质通报》2014,33(1):9-18

哈拉奇组为新疆阿合奇县开展1∶5万区域地质矿产调查工作时建立的岩石地层单位,分布在新疆阿合奇县哈拉奇地区北部,主要为一套深水碳酸盐沉积,与该区南部属碳酸盐台地沉积的康克林组在岩性、岩石组合及古生物组合上形成明显的差别。通过对该组重力流成因的生物屑砾屑灰岩中古生物化石的研究,确定其 带为Triticites带和Pseudoschwagerina带,进而确定该组地质时代为晚石炭世—早二叠世,与南区康克林组为同时异相沉积。哈拉奇组的建立完善了该地区上石炭统—下二叠统的地层系统,确定了该地区晚石炭世—早二叠世台地边缘斜坡相的存在,对塔西北地区晚石炭世—早二叠世岩相古地理研究具有重要意义。  相似文献   

江南造山带西段桂北龙胜地区金车辉长岩矿物化学研究及其地质意义     

寇彩化  刘燕学  李廷栋  丁孝忠  张恒 《岩石矿物学杂志》2017,36(1):20-35

桂北龙胜地区位于江南造山带西段,本文利用电子探针对桂北龙胜地区金车辉长岩单斜辉石和斜长石进行了详细的矿物学和矿物化学研究,研究表明单斜辉石的成分为Wo27~28En47~57Fs15~22,属于普通辉石,斜长石的成分为An1.35~9.05Ab90.34~97.45Or0.36~1.05,为钠长石。单斜辉石温压估算结果显示,其形成温度为1 250~1 350℃,该温度基本与软流圈地幔温度(1 280~1 350℃)相当,其形成压力为1.31~2.25 GPa,对应深度为43.2~74.3 km。单斜辉石成分特征指示金车辉长岩为板内拉斑玄武岩,结合区域地质特征,推测金车辉长岩是裂谷构造背景下软流圈地幔物质上涌并发生减压熔融的产物。  相似文献   

湘西通道地区新元古代长界橄榄辉石岩中单斜辉石矿物学特征及其板内裂谷成因论证     

寇彩化  刘燕学  李廷栋  丁孝忠  张恒  陆济璞 《地质论评》2017,63(4):881-893

湘西通道地区长界橄榄辉石岩主要组成矿物为单斜辉石、橄榄石和斜长石,还具有少量的Ti—Fe氧化物。本文利用电子探针对江南造山带西段湘西通道地区长界橄榄辉石岩单斜辉石进行了详细的矿物学研究,研究结果表明单斜辉石属于顽透辉石和普通辉石。长界橄榄辉石岩单斜辉石较富镁而贫铁,并且还具有高硅、贫碱、低钙的特征,其母岩浆属于拉斑玄武系列。单斜辉石温压计算结果显示,橄榄辉石岩的形成温度为1260～1383℃,压力为1.5～2.6GPa,深度为50～86km,平均深度为73km。整体来看,长界橄榄辉石岩形成的温度基本与软流圈地幔的温度(1280～1350℃)相当,其形成深度为约73km的地幔深处,且在这种温压条件下,软流圈地幔可以发生减压熔融。单斜辉石的成分特征显示示长界橄榄辉石岩是板内拉斑玄武岩,指示其构造背景为裂谷环境。另外,单斜辉石具低的Al_2O_3(0.02%～5.51%)、TiO_2(0～0.46%)和Na_2O(0.01%～1.44%)的特征,这可能是单斜辉石寄主岩石岩浆源区受到俯冲熔体/流体的交代改造作用所导致。结合作者和前人的研究结果,我们推测长界橄榄辉石岩源区为软流圈地幔,其形成可能与裂谷作用导致软流圈物质上涌并发生熔融有关,且在形成长界橄榄辉石岩之前,软流圈地幔已经遭受过俯冲熔体/流体的交代改造作用。  相似文献   

Characteristics and Natural Gas Origin of Middle−Late Triassic Marine Source Rocks of the Western Sichuan Depression, SW China     

SUN Tengjiao  LUO Xiaoping  QING Hairuo  KOU Xueling  SHENG Zhongming  XU Guosheng  ZUO Yinhui 《《地质学报》英文版》2020,94(2):376-398

A scientific exploration well(CK1) was drilled to expand the oil/gas production in the western Sichuan depression, SW, China. Seventy-three core samples and four natural gas samples from the Middle–Late Triassic strata were analyzed to determine the paleo-depositional setting and the abundance of organic matter(OM) and to evaluate the hydrocarbon-generation process and potential. This information was then used to identify the origin of the natural gas. The OM is characterized by medium n-alkanes(n C_(15)–n C_(19)), low pristane/phytane and terrigenous aquatic ratios(TAR), a carbon preference index(CPI) of ～1, regular steranes with C_(29) C_(27) C_(28), gammacerane/C_(30) hopane ratios of 0.15–0.32, and δD_(org) of-132‰ to-58‰, suggesting a marine algal/phytoplankton source with terrestrial input deposited in a reducing–transitional saline/marine sedimentary environment. Based on the TOC, HI index, and chloroform bitumen "A" the algalrich dolomites of the Leikoupo Formation are fair–good source rocks; the grey limestones of the Maantang Formation are fair source rocks; and the shales of the Xiaotangzi Formation are moderately good source rocks. In addition, maceral and carbon isotopes indicate that the kerogen of the Leikoupo and Maantang formations is type Ⅱ and that of the Xiaotangzi Formation is type Ⅱ–Ⅲ. The maturity parameters and the hopane and sterane isomerization suggest that the OM was advanced mature and produced wet–dry gases. One-dimensional modeling of the thermal-burial history suggests that hydrocarbon-generation occurred at 220–60 Ma. The gas components and C–H–He–Ar–Ne isotopes indicate that the oilassociated gases were generated in the Leikoupo and Maantang formations, and then, they mixed with gases from the Xiaotangzi Formation, which were probably contributed by the underlying Permian marine source rocks. Therefore, the deeply-buried Middle–Late Triassic marine source rocks in the western Sichuan depression and in similar basins have a great significant hydrocarbon potential.  相似文献   

中国南海天然气水合物第二次试采主要进展          下载免费PDF全文

叶建良  秦绪文  谢文卫  卢海龙  马宝金  邱海峻  梁金强  陆敬安  匡增桂  陆程  梁前勇  魏士鹏  于彦江  刘春生  李彬  申凯翔  史浩贤  卢秋平  李晶  寇贝贝  宋刚  李博  张贺恩  陆红锋  马超  董一飞  边航 《中国地质》2020,47(3):557-568

泥质粉砂型天然气水合物被认为是储量最大开采难度亦最大的水合物储层,2017年南海天然气水合物试采,初步验证了此类水合物储层具备可开采性。在总结前次试采认识的基础上,对试采矿体进行优选、精细评价、数值与试验模拟和陆地试验,中国地质调查局于2019年10月—2020年4月在南海水深1225 m神狐海域进行了第二次天然气水合物试采。本次试采攻克了钻井井口稳定性、水平井定向钻进、储层增产改造与防砂、精准降压等一系列深水浅软地层水平井技术难题,实现连续产气30 d,总产气量86.14×104m3,日均产气2.87×104m3,是首次试采日产气量的5.57倍,大大提高了日产气量和产气总量。试采监测结果表明,整个试采过程海底、海水及大气甲烷含量无异常。本次成功试采进一步表明,泥质粉砂储层天然气水合物具备可安全高效开采的可行性。  相似文献   

大兴安岭西缘罕布庙地区玛尼吐组火山岩锆石U- Pb年龄、地球化学特征及构造意义     

邵永旭  李钢柱  姜海蛟  许展  寇帅  连琛芹  黄磊 《地质学报》2020,94(12):3590-3606

大兴安岭西缘内蒙古罕布庙地区玛尼吐组火山岩主要由安山岩和英安岩组成。通过LA- ICP- MS锆石U- Pb年代学方法对玛尼吐组火山岩进行精确定年,获得安山岩结晶年龄为153. 4±0. 8Ma（MSWD=0. 29),英安岩结晶年龄为155. 6±0. 6Ma（MSWD=0. 12),表明这套火山岩的形成时代为晚侏罗世。罕布庙地区玛尼吐组火山岩具有富碱、过铝质的特征,属高钾钙碱性系列岩石。样品稀土元素总量介于122. 72×10-6~416. 68×10-6,不同类型岩石微量元素和稀土元素组成总体相似,轻重稀土元素分馏明显\[(La/Yb)N=10. 85~60. 04\],具弱负Eu异常（δEu=0. 71~0. 87),富集Rb、Ba等大离子亲石元素和轻稀土元素,亏损Nb、Ta、P、Ti、Y等高场强元素,具有陆缘弧岩浆岩的地球化学特征。新的年代学和岩石地球化学证据指示罕布庙地区玛尼吐组火山岩形成于古太平洋板块向欧亚大陆下俯冲的陆缘弧环境。  相似文献   

砂土地基中箱筒型防波堤基础稳定性试验研究与机理分析     

周超  寇海磊  闫正余  刁闻宙  周楠  陈琦 《海洋工程》2021,39(6):47-56

箱筒型防波堤基础是一种能够适应复杂海况的新型基础形式。利用室内模型试验对箱筒型防波堤基础在水平静载荷及水平循环荷载作用下的稳定特性进行了研究。结果表明：砂性土地基中箱筒型防波堤基础破坏可分为准弹性、塑性及破坏三个阶段,以荷载位移曲线出现明显拐点判断箱筒型防波堤基础极限承载力约为0.08 kN。以循环过程中施加荷载与静载荷水平极限承载力比值定义荷载循环比ζ_b,当ζ_b=0.5、ζ_b=1.0时,防波堤基础前10次累计位移最为明显,分别占总循环累计位移的96.70%、91.88%,这主要是由于砂土发生剪胀,土颗粒重新排列所致;而后40次循环累计位移不明显,分别占总循环累计位移的3.30%、8.12%,此时土体发生剪缩,土颗粒之间致密化。当ζ_b=0.5时,循环结束后防波堤基础抗滑移系数K₁、抗倾覆系数K₂分别为1.619、3.372;当ζ_b=1.0时,抗滑移系数K₁、抗倾覆系数K₂分别为0.839、-18.063,说明ζ_b=0.5循环荷载作用下砂性土地基防波堤基础稳定性良好,但ζ_b=1.0循环加载时,基础首先发生滑移破坏进而发生严重的倾覆破坏。  相似文献   

Improving Airgun Signal Detection with Small-Aperture Seismic Array in Yunnan   总被引：1，自引：1，他引：0  

WANG Weijun  ZHOU Qingyun  KOU Huadong  LIU Guiping  ZHU Hongbo  YAN Kun 《中国地震研究》2019,33(2):248-264

Repeating airgun sources are eco-friendly sources for monitoring the changes in the physical properties of subsurface mediums, but their signals decay quickly and are buried in the noises soon after traveling short distances. Stacking waveforms from different airgun shots recorded by a single seismic station (shot stacking) is the most popular technique to detect weak signals from noisy backgrounds, and has been widely used to process the data of Fixed Airgun Signal Transmission Stations (FASTS) in China. However, shot stacking sacrifices the time resolution in monitoring to recover a qualified airgun signal by stacking many shots at distance stations, and also suffers from persistent local noises. In this paper, we carried out several small-aperture seismic array experiments around the Binchuan FAST Station (BCFASTS) in Yunnan Province,China, and applied the array technique to improve airgun signal detection. The results show that seismic array processing combining with shot stacking can suppress seismic noises more efficiently, and provide better signal-to-noise ratio (SNR) and coherent airgun signals with less airgun shots. This work suggests that the array technique is a feasible and promising tool in FAST to increase the time resolution and reduce noise interference on routine monitoring.  相似文献   

海水冲厕技术研究与应用进展   总被引：1，自引：0，他引：1  

寇希元  张雨山  王静 《海岸工程》2009,28(2):83-89

推广海水冲厕是解决沿海城市淡水资源紧缺的有效措施之一。综述了近年来我国海水冲厕技术的研究现状和发展趋势，介绍了海水冲厕在香港的应用现状和在青岛等内地沿海城市的推广应用情况。总结并探讨了海水冲厕推广应用存在的问题及解决这些问题的应对措施。  相似文献