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31.
瑞雷波勘探在地下洞穴探测中的应用 总被引:4,自引:0,他引:4
利用瑞雷波勘探方法进行地下洞穴探测,在实际处理过程中,对场地所测得的面波频散曲线进行分类、归纳,并利用动力触探曲线对各种特征曲线所反映的地下洞穴情况进行标定,从而确定整个测区洞穴的空间分布规律。 相似文献
32.
33.
Trace Elements in Fluid Inclusions in the Carlin—Type Gold Deposits,Southwestern Guizhou Province 总被引:2,自引:1,他引:2
Fluid inclusions in quartz from the Lannigou and Yata Carlin-type gold deposits in southwestern Guizhou were analyzed by inductively coupled plasma-mass spectrometry for their trace elements(Co,Ni,Cu,Pb,Zn,Pt,etc.).The results show that quartz fluid inclusions entrapped at different ore-forming stages contain higher Co,Ni,Cu,Pb and Zn.It has been found for the first time that the ore-forming fluids responsible for the Carlin-type gold deposits are rich in Pt.From this it can be concluded that basic volcanic rocks seem to be one of the important sources of ore-forming materials for the Carlin-type gold deposits. 相似文献
34.
中国东北区二叠纪和早三叠世地层 总被引:4,自引:1,他引:4
本文运用裂陷槽理论,提出了早二叠世地层发育于大石寨、大河深和庙岭三个裂陷槽中。晚二叠一早三叠世则以陆相凹陷沉积为特征,发育于兴安岭、张广才岭及完这山三个凹陷内。 相似文献
35.
全新世岱海流域化学风化及其对气候事件的响应 总被引:12,自引:0,他引:12
通过对岱海 12.08 m沉积岩芯 210Pb和 AMS- 14C精确定年及地球化学、物理指标的综合分析,重建了包括 8.2 ka冷期、中世纪暖期 (MWP)和小冰期 (LIA)等典型气候事件在内的全新世以来所经历的化学风化及其环境演化过程.全新世早-中期 (9.0~ 3.5 ka),岱海流域处于温暖湿润气候环境,主要环境特征表现为流域化学风化显著增强、生物生产力逐步提高、湖泊水位大幅度抬升.在 7.90~ 8.25 ka期间存在一次冷气候事件,其发生时间与来自湖沼、海洋、生物组合和极地冰芯等在内的全球环境记录基本一致,具体表现为流域化学风化减弱、湖泊生产力降低以及湖泊水位下降. 2.5 ka以来,岱海沉积物中环境指标的显著变化,表明进入气候波动更频繁的新冰期.岱海沉积物中的指标变化也展示了本世纪以来的气候增暖过程,但其化学风化强度还没有达到 MWP的程度. 相似文献
36.
The changes of vegetation cover in Ejina Oasis based on water resources redistribution in Heihe River 总被引:1,自引:0,他引:1
Wang Yaobin Feng Qi Si Jianhua Su Yonghong Chang Zongqiang Xi Haiyang 《Environmental Earth Sciences》2011,64(7):1965-1973
The Ejina Oasis (EO), located in arid northwest China, is a typical arid area in the world. The ecosystem in the oasis has
become worse since the 1990s. However, it began to improve after the Chinese government took the mandatory measure to redistribute
the water in Heihe in 2000. To understand this change, the remote sensing images in 1990, 2000 and 2006 were selected, and
exertion related Land Use/Cover Change (LUCC) model was employed. Results showed that: (1) non-vegetation cover was the main
body of the vegetation cover in oasis, showing a trend of increase at the beginning and diminution later, while low, medium
and high vegetation cover was the other way around; (2) the area of low, medium and high vegetation cover in 2006 was less
than that in 1990; the status and trend index P
t of oasis vegetation cover was 0.62 in 1990–2000, which means that the oasis ecosystem of Ejina was getting worse and was
under an unbalanced status; P
t was 0.27 in 2000–2006 indicating that the oasis ecosystem was restored obviously and the whole system tended to be balanced;
(3) all of these changes should be attributed to the water resources redistribution in Heihe River, which played a leading
role, as well as the measures and relevant policies taken by the local government, which promoted the rapid recovery of the
medium and high vegetation. 相似文献
37.
38.
在安徽定远东兴盐矿勘探中,通过采用地震反射波法与钻孔的对比分析,充分说明地震反射波法在第三系地层中寻找石膏矿、岩盐等沉积型矿藏有着良好的应用前景。 相似文献
39.
40.
Impact of Montmorillonite and Calcite on Release and Adsorption of Cyanobacterial Fatty Acids at Ambient Temperature 总被引:1,自引:0,他引:1
Minerals might act as important sorbents of sedimentary organic matter and reduce biodegradation, which favors the formation of hydrocarbon source rocks in the earth's history. Since most organic matter is degraded during the sinking process, at ambient temperature, it is important to investigate the adsorption capacity of different minerals during this process, to assess the organic loss from primary productivity to sedimentary organic matter. In this study, montmorillonite and calcite have been selected to study the impact of different minerals on the release, adsorption, and deposition of cyanobacterial (Synechococcus elonpata) fatty acids (FAs) at ambient temperature. Gas chromatography (GC), gas chromatography-mass spectrometry (GC-MS) have been utilized to detect the variation in fatty acids. Primary results suggest that minerals have a different impact on dissolved organic matter. Montmorillonite can specifically enhance the release of fatty acids from cyanobacterial cells by lowering the pH values of the solution. The adsorption of the dissolved organic matter by montmorillonite will also be enhanced under a lower pH value. Conjunction of fatty acids with montmorillonite to form a complex will favor the sinking and preservation of these organics. Selective adsorption is observed among fatty acids with different carbon numbers. In contrast, calcite does not show any impact on the release and adsorption of organic matter even though it is reportedly capable of acting as a catalyst during the transformation of organic matter at high temperature. The primary data bridge a link between primary productivity and sedimentary organic matter, suggesting the relative importance of claystones in the formation of hydrocarbon source rocks in the earth's history. 相似文献