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61.
The meta-basic volcanic rocks in the Tengtiaohe Zone yield zircon U–Pb ages of 258.8±2.5 Ma and 259.2±1.8 Ma, respectively which agree with the ages of flood basalts of ELIP and are similar to the basaltic rocks and komatiites from the Song Da Zone in northern Vietnam. The results suggest that the age of meta-basic volcanic rocks is Late Permian, rather than the Early Permian or Early Carboniferous ages as previously inferred. Most meta-basic volcanic rocks are strongly enriched in LREEs relative to HREEs and display trace element patterns similar to the ELIP high-Ti basalts, and are enriched in LILEs with negative Sr anomalies. Their initial ~(87)Sr/~(86) Sr ratios range from 0.705974 to 0.706188 and εNd(t) from-0.82 to-2.11. Their magmas were derived from an enriched and deep mantle source without significant crustal contamination. These meta-basic volcanic rocks formed in ELIP. Therefore, the Tengtiaohe Zone is not an ophiolite zone and can link to the Song Da Zone in northern Vietnam.  相似文献   
62.
关于峨眉山大火成岩省一些问题的研究现状   总被引:4,自引:1,他引:3  
峨眉山大火成岩省(ELIP)位于扬子板块西缘,是我国唯一被国际学术界认可的大火成岩省,受到国内外学者的广泛关注。主要围绕峨眉山玄武岩喷发前的隆升剥蚀情况、喷发时限、地幔柱的轴部位置等争议性问题进行探讨,总结了前人的研究成果。由于地幔柱和岩石圈之间相互作用的复杂性,加之地幔柱模型的不完善,峨眉山地幔柱活动在地表的真实响应也许更复杂。在今后的研究中,应该加强不同学科间的相互合作,着重研究地球深部动力学过程以及地球系统各圈层的相互作用。  相似文献   
63.
新疆阜康市白杨河矿区煤层气开发利用先导性示范工程是新疆第一个煤层气示范工程项目。白杨河矿区总体构造为向南倾斜的单斜构造,地层倾角大,煤层多且间距大。该示范工程开发方案主要井型为丛式井。经过多年钻井实践,丛式井钻井技术在鄂尔多斯盆地东缘煤层气区块已经非常成熟,初步形成了一套适合该地区煤层气开发的丛式井钻井技术。由于白杨河矿区地质条件与鄂尔多斯盆地东缘各区块相比差异大,特别是存在地层倾角大、煤层多且间距大等地质特点,因此不能完全照搬原有的丛式井钻井技术。本文依据白杨河矿区地质资料,分析了白杨河矿区煤层气丛式井钻井难点,对解决该区块钻井难点的技术对策和攻关思路进行了总结与阐述,初步形成了一套适合白杨河矿区大倾角厚煤层的丛式井钻井技术。  相似文献   
64.
朱恒银  王强  张正  蔡正水 《探矿工程》2016,43(10):160-164
根据页岩气、煤层气勘探对钻探技术的特殊要求,进行了大直径绳索取心技术的探索研究。文中重点介绍了加重管组合式绳索取心钻具的结构、作用原理及特点,以及施工试验效果。通过施工实践的启示,对大直径绳索取心技术的发展提出了几点认识。  相似文献   
65.
We present a pattern-based regionalization of the conterminous US – a partitioning of the country into a number of mutually exclusive and exhaustive regions that maximizes the intra-region stationarity of land cover patterns and inter-region disparity between those patterns. The result is a discretization of the land surface into a number of landscape pattern types (LPTs) – spatial units each containing a unique quasi-stationary pattern of land cover classes. To achieve this goal, we use a recently developed method which utilizes machine vision techniques. First, the entire National Land Cover Dataset (NLCD) is partitioned into a grid of square-size blocks of cells, called motifels. The size of a motifel defines the spatial scale of a local landscape. The land cover classes of cells within a motifel form a local landscape pattern which is mathematically represented by a histogram of co-occurrence features. Using the Jensen–Shannon divergence as a dissimilarity function between patterns we group the motifels into several LPTs. The grouping procedure consists of two phases. First, the grid of motifels is partitioned spatially using a region-growing segmentation algorithm. Then, the resulting segments of this grid, each represented by its medoid, are clustered using a hierarchical algorithm with Ward’s linkage. The broad-extent maps of progressively more generalized LPTs resulting from this procedure are shown and discussed. Our delineated LPTs agree well with the perceptual patterns seen in the NLCD map.  相似文献   
66.
Deccan volcanic sequences( DVS) in the central Deccan volcanic province( CDVP) are designated as Sahyadri Group having ~ 500 m thick lava pile associated with multiple sedimentary beds at different stratigraphic levels. In the eastern part of CDVP between the latitude 19 °55 '--20 °25 ' N and the longitudes 78 °15 '--78 °30 ' E,palynological investigation of the intertrappean sedimentary beds at five stratigraphic levels was carried out. The study was basically aimed for tracking the floral and environmental changes across the Deccan transition. The resulting finds indicate that the intertrappean sediments at the lowest stratigraphic level between the earliest lava flows are characterized by presence of marker Maastrichtian palynomorphs- Gabonisporis vigourouxii,Aquilapollenites bengalensis,Azolla cretacea and Farabeipollis associated with triporate and tricolpate pollen grains,phytoliths of Oryzeae of Poaceae family and peridinoid dinoflagellate cysts. The increasing volcanism deteriorated the existing flora as evident by absence of pollen-spores and presence of only structured biodegraded organic matter,fungal spores,acritarchs and algal( Botryococcus) remains in the sediments of higher-up in the sequence. For chronostratigraphic constraints on the lava flows magnetic polarity of the flows bracketing the intertrappean beds was investigated. The results indicated presence of N-R-N-R magnetic polarity in the basal lava pile that are interpreted as representing the magnetochron C30 N to C28 R( Maastrichtian-Paleogene). The floral change begins with the onset of volcanism in the chron C30 N and floral deterioration is observed in C29 N with increasing volcanism and it is only in the chron C28 R( Danian) that some evidence of recovery of flora is recorded. The current study shows that in eastern part of CDVP the post Cretaceous-Paleogene boundary eruptions represent the main phase of eruptions that triggered deterioration of the flora.  相似文献   
67.
金瑞佳  滕斌  吕林 《海洋工程》2016,34(5):11-19
在深海中系泊的海洋平台,如Spar平台,水下部分为带有系泊的圆柱结构,其水平方向运动响应往往具有较低的自振频率,容易在低频波浪力(源于非线性的差频效应)作用下发生共振响应,使结构发生大幅水平慢漂。当浮体的瞬时位置大幅偏离初始位置时,基于初始平衡位置的摄动展开法会存在较大误差。针对这一问题,采用两次展开方法,对大幅慢漂运动开展时域模拟研究。对双色波作用下自由漂浮圆柱的大幅运动响应问题进行数值分析,并与采用基于初始平衡位置的摄动展开法的计算结果进行了对比。结果表明,采用新的两次展开法可以计算出波浪遭遇频率的变化和波浪漂移阻尼,而这无法从基于初始平衡位置的常规摄动展开法中得到,体现了两次展开法在分析大幅慢漂问题上的优势。  相似文献   
68.
Paleoseismological studies confirm that the Uimon basin is thrust by its northern mountain border along the active South Terekta fault. The latest motion along the fault in the 7-8th centuries AD induced an earthquake with a magnitude of Mw= 7.4-7.7 and a shaking intensity of I = 9-11 on the MSK-64 scale. The same fault generated another event (M > 7, I = 9-10), possibly, about 16 kyr ago, which triggered gravity sliding. The rockslide dammed the Uimon valley and produced a lake, where lacustrine deposition began about 14 ± 1 kyr ago, and a later M > 7 (I = 9-10) earthquake at ~ 6 ka caused the dam collapse and the lake drainage. Traces of much older earthquakes that occurred within the Uimon basin are detectable from secondary deformation structures (seismites) in soft sediments deposited during the drainage of a Late Pleistocene ice-dammed lake between 100 and 90 ka and in ~ 77 ka alluvium. The magnitude and intensity of these paleoearthquakes were at least M > 5.0-5.5 and I > 6-7.  相似文献   
69.
蒋太平  李果民  肖华  沈林江 《探矿工程》2021,48(S1):269-274
为了获取参数井压裂设计的相关参数,需要对井眼进行阵列声波测井和微侧向电阻率测井,需要采取大直径岩心进行力学实验。采用固体岩心钻探取心工艺,钻孔口径难以达到物探测井仪器入井要求,岩心直径也不能满足实验要求,必须采用大口径取心工艺才能满足设计要求。同时,常规取心工艺难以满足页岩气勘探对岩心(页岩或者煤心)提升时间的要求,绳索取心工艺在这方面优势明显。本篇介绍了大口径绳索取心工艺在页岩气地质调查井川蔺参1井的成功应用,根据大口径绳索取心钻具的结构特点,结合目的层岩性特征,总结了合理的取心钻进工艺参数和技术保障措施,取得了较好的效果。  相似文献   
70.
以深圳某项目桩基础施工为依托,综合考虑地质特点和施工工艺要求,对超大超深灌注桩在花岗岩地层施工开展了相关研究,并将研究成果应用到实际施工中,有效地解决了该类型桩基础施工中的难点,保证了项目的顺利实施,为后续类似项目提供了参考依据。  相似文献   
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