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71.
印度共和国是印度板块的主体,也是冈瓦纳大陆的重要组成部分,主要由七个古老克拉通(陆块群)、分隔克拉通的活动带与盆地等构成。自北向南依次为:①喜马拉雅活动带,主要为具有元古代基底的古近纪-新进纪活动带;②印度河-恒河平原过渡带(山前坳陷带),主要由为第四系、古近系-新进系和第四系冲积物构成;③印度半岛克拉通,主要由西塔尔瓦尔、东塔尔瓦尔、巴斯塔、辛本,本德尔坎德、阿拉瓦利和印度南部麻粒岩地体等7个太古宙陆块(或次级克拉通)群构成;④萨德布尔活动带;⑤东高止山活动带;⑥德干高原玄武岩省(LIP)(图1)。 相似文献
72.
运用高压压汞、液氮吸附及渗透率测试等实验,利用极差、突进系数、变异系数等参数,表征煤系页岩孔渗特征及孔隙层间非均质性,分析孔隙层间非均质性主控因素。结果表明:河南义马地区上、下石盒子组泥页岩微孔与小孔较为发育,山西组大孔较为发育,分别提供了气体吸附附着面积和储存运移空间;上石盒子组孔容与孔径相对偏差最小,孔隙分布均匀,山西组比表面积相对偏差最小,表面积分布均匀;随围压增大,渗透率不断降低,且满足负指数相关关系;渗透率级差、突进系数和变异系数显示下石盒子组渗透率非均质性较弱,山西组渗透率非均质性很弱,更易于压裂开发。非均质性宏观上主要受沉积物质组成和构造改造作用影响,微观上受成岩演化影响。 相似文献
73.
在前人资料和野外勘查的基础上对祁连山及邻区贵德盆地、循化—化隆盆地、同仁盆地、西宁盆地、门源盆地、临夏盆地、兰州盆地、定西盆地、天水盆地、肃北盆地、酒泉盆地、玉门盆地、张掖盆地、武威盆地、哈拉湖盆地、苏里盆地、木里盆地、民和盆地、共和盆地、青海湖盆地及柴达木等20余个盆地的第四纪地层进行了研究。以祁连山第四纪构造地貌演化、盆地沉积序列、古生物及古气候特征为地层分区依据,对祁连山及邻区第四纪地层进行了地层分区,并对部分地层名称做了厘定或统一。祁连山及邻区第四纪沉积特征总体为东部(主要为陇中地区)黄土分布广泛,堆积了世界上最厚的黄土地层;北部(河西走廊地区)冲洪积扇堆积及风沙发育;南部(柴北盆地)以冲洪积-湖积为主,晚更新世以来发育风成沙及黄土;共和盆地由湖泊转向冲积扇和风沙沉积;青海湖盆延续至今;中西部高山及山间盆地冰碛、冰水堆积以及河流阶地堆积发育。根据上述特征及划分原则,将祁连山及邻区第四纪地层区划分为:兰州—西宁地层区,贵德地层区,酒泉—张掖地层区,柴北地层区,共和地层区,青海湖地层区及肃北—门源地层区。 相似文献
74.
75.
油气上窜速度对钻井施工中下一步施工方案的制定具有重要参考价值。文章在总结分析前人经验的基础上结合现场施工实际对传统油气上窜速度计算公式加以修正,并对修正后的公式中涉及到的参数进行了逐一分析,在不影响正常施工工序的条件下使公式中各参数取值准确性进一步提高。通过现场工程测试,该方法简单实用且计算准确性较高。该计算方法在保证计算结果准确性的同时,也具备较强的现场可操作性,通过大量的实践检验后可进一步推广。 相似文献
76.
在实验室条件下,对大连蜈蚣藻(Grateloupia dalianensis H.W.Wang et D.Zhao)的孢子早期发育、盘状体的形成和直立枝生长进行了详细研究,对其生活史进行了详细观察,并进行了温度和光照强度对孢子发育影响的研究。结果表明:(1)孢子发育类型为间接盘状体型;(2)生活史由雌、雄配子体、四分孢子体和果孢子体三相世代组成,配子体与孢子体形态相同,属于同型世代交替,与属模蜈蚣藻(G.filicina)一致;(3)温度对盘状体和直立枝生长均有影响,最适温度均为16℃;(4)光照强度对盘状体和直立枝生长均有影响,最适光照强度分别为7 500 lx和10 000 lx。 相似文献
77.
This paper presents an artificial neural network (ANN)-based response surface method that can be used to predict the failure probability of c-φ slopes with spatially variable soil. In this method, the Latin hypercube sampling technique is adopted to generate input datasets for establishing an ANN model; the random finite element method is then utilized to calculate the corresponding output datasets considering the spatial variability of soil properties; and finally, an ANN model is trained to construct the response surface of failure probability and obtain an approximate function that incorporates the relevant variables. The results of the illustrated example indicate that the proposed method provides credible and accurate estimations of failure probability. As a result, the obtained approximate function can be used as an alternative to the specific analysis process in c-φ slope reliability analyses. 相似文献
78.
The characteristics of rill development and their effects on runoff and sediment yield under different slope gradients 总被引:8,自引:0,他引:8
Rill formation is the predominant erosion process in slope land in the Loess Plateau, China. This study was conducted to investigate rill erosion characteristics and their effects on runoff and sediment yielding processes under different slope gradients at a rate of 10°, 15°, 20° and 25° with rainfall intensity of 1.5 mm min-1 in a laboratory setting. Results revealed that mean rill depth and rill density has a positive interrelation to the slope gradient. To the contrary, width-depth ratio and distance of the longest rill to the top of the slope negatively related to slope gradient. All these suggested that increasing slope steepness could enhance rill headward erosion, vertical erosion and the fragmentation of the slope surface. Furthermore,total erosion tended to approach a stable maximum value with increasing slope, which implied that there is probably a threshold slope gradient where soil erosion begins to weaken. At the same time, the correlation analysis showed that there was a close connection between slope gradient and the variousindices of soil erosion: the correlation coefficients of slope gradient with maximal rill depth, number of rills and the distance of the longest rill from the top of the slope were 0.98, 0.97 and-0.98, respectively,indicating that slope gradient is the major factor of affecting the development of rills. Furthermore,runoff was not sensitive to slope gradient and rill formation in this study. Sediment concentration,however, is positively related to slope gradient and rill formation, the sediment concentrations increased rapidly after rill initiation, especially. These results may be essential for soil loss prediction. 相似文献
79.
Guangjun Wang Ermeng Yu Zhifei Li Deguang Yu Haiying Wang Wangbao Gong 《中国海洋大学学报(英文版)》2016,15(3):495-501
The present study was conducted to evaluate the feasibility of replacing fish meal (FM) with bioactive peptides (BPs) in diet of white shrimp (Litopenaeus vannamei). The changes in growth performance, body composition, non-specific immunity, and water quality were examined after the shrimp were fed four diets, in which 0% (control), 33.3%, 66.7% and 100% of FM was replaced by BPs, respectively. The groups were designated as Con, 1/3BPs, 2/3BPs, and 3/3BPs. A total of 720 shrimp with an initial body weight of 1.46 ± 0.78 g were fed the experimental diets for 56 days. The results revealed that: 1) the weight gain rate (WGR) in 1/3BPs, 2/3BPs, and 3/3BPs was significantly higher than that in Con (P < 0.05), while no significant difference was found on survival rate and feed conversion ratio (FCR); 2) the whole-body crude protein (CP) and crude lipids (CL) were significantly different among groups, while there was no significant difference between crude ash and phosphorus contents; 3) the levels of acid phosphatase (ACP), lysozyme (LZM), superoxide dismutase (SOD), phenol oxidase (PO) and bactericidal activity increased significantly with the inclusion of BPs; 4) in terms of water quality, no significant difference was found in pH and dissolved oxygen among diets during the whole experimental period. Moreover, even though nitrite and ammonium levels tended to increase with time, there was no significant difference among groups. The results indicated that BPs is an applicable alternative of protein source, which can substitute FM in the diets of L. vannamei; it is able to effectively promote growth performance and improve immunity. Moreover, BPs in the diets had no negative impact on water quality. 相似文献
80.
东昆仑造山带晚古生代—早中生代由于布青山-阿尼玛卿洋的俯冲发育有大量岛弧型花岗岩类。选取东昆北巴隆地区朝火鹿陶勒盖花岗闪长岩体寄主岩和闪长质暗色微粒包体进行了岩相学、LA-ICP-MS锆石U-Pb年代学及地球化学研究。结果表明,岩体寄主岩的结晶年龄为242.3±1.3Ma,暗色微粒包体结晶年龄为241.2±0.8Ma,显示其形成于中三叠世;寄主岩和暗色微粒包体A/CNK值介于0.86~1.06之间,为准铝质-弱过铝质;稀土元素总量分别为119×10~(-6)~170×10~(-6)、189×10~(-6),稀土元素配分模式显示右倾型,具有负Eu异常;岩石富集Rb、Ba、Th等大离子亲石元素,亏损Nb、Ta、Ti等高场强元素,具有弧岩浆岩特征。野外及岩相学特征均显示包体为基性岩浆进入酸性岩浆快速冷凝形成的,为俯冲板片断离导致幔源岩浆上侵形成的岩浆混合作用的产物,是布青山-阿尼玛卿洋俯冲晚期的岩浆记录。 相似文献