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排序方式: 共有413条查询结果,搜索用时 218 毫秒
81.
在实际煤田地球物理勘探中,常规的地面地震勘探技术无法对煤层中的小断层、陷落柱、夹矸等微幅构造体进行精细的探测。相比于地面地震勘探,槽波地震勘探直接在煤层中激发,能量强,范围大,能够精确探测煤层中的微幅构造体。笔者等针对反射槽波地震数据的特征,给出了一种有效的反射槽波地震数据精细处理技术和流程,通过对频散分析以及槽波包络叠加等关键技术进行试验研究,提高反射槽波地震数据的成像精度,进而更准确地识别煤层中小断层等微幅构造。实际煤田反射槽波的应用试验表明,反射槽波勘探准确识别出煤层中的小断层构造,验证了反射槽波勘探技术的实用性以及本文反射槽波地震数据处理技术的有效性。 相似文献
82.
We investigated the meta-gabbronorites in Liangcheng and used detailed petrography, geochemistry, zircon geochronological and in-situ Hf isotopic studies to clarify their formation and metamorphic ages, petrogenesis, tectonic setting and provide constraints on the tectonic evolution of Khondalite Belt(KB). The zircon U-Pb dating results show that the meta-gabbronorites crystallized at ~1.94 Ga and were metamorphosed at ~1.91–1.89 Ga. They can be subdivided into the low-Mg and high-Mg groups. The... 相似文献
83.
ZHAO Yawen WU Guanghui YI Yan CHEN Yongquan WU Yonghong JING Bing WANG Jian 《《地质学报》英文版》2023,97(5):1523-1537
Early Cambrian shale is an important petroleum source rock around the world. Because of little drilling data and poor seismic data, until recently, organic matter enrichment of the Lower Cambrian Yuertusi and Xishanbulake formations shale is still an enigma in the Tarim Basin, northwestern China. Total organic carbon (TOC), major and trace element data of Cambrian shale samples from five boreholes have been analyzed to decipher the mechanism of the organic matter enrichment. The results show that the shales deposited in the western restricted intraplatform have much higher TOC contents (3.2%–19.8%, on average 11.0%) than those from the eastern basin (2.2%–10.2%, on average 4.5%). The paleoproductivity proxies (Ba, Ba/Al, P/Al) in the western restricted platform are much higher than those in the eastern basin. The trace element indicators such as V/Cr, Ni/Co, Mo–TOC and MoEF–UEF suggest an anoxic environment across the basin, but a more restricted environment in the western intraplatform. The paleoproductivity rather than anoxic condition and hydrothermal activity are concluded to have resulted in the differentiation of the organic matter enrichment from the western intraplatform to eastern basin in the early Cambrian shales; the restricted environment was favorable for paleoproductivity and preservation of organic matter. 相似文献
84.
高纯石英具有重要的战略地位,是高新技术产业的基础原材料。本文对高纯石英原料的特征和矿床成因研究方法进行了系统的归纳。通过观察石英岩相学特征,分析矿物包裹体及流体包裹体的数量、大小、化学成分、存在形式和分布状态,以及SiO2和微量杂质元素的含量和赋存状态,可以研究高纯石英原料的矿物学特征;通过Ar Ar同位素定年可以计算高纯石英原料矿床的成矿年龄;通过H—O同位素测试,Ti、Al、Ge、Li等微量元素含量分析,可以研究高纯石英原料矿床的成矿物质来源;通过分析流体包裹体的均一温度、盐度、化学组成等特征以及SEM CL微结构观察,可以研究高纯石英原料矿床的成矿作用过程。在此基础上,本论文对我国高纯石英行业的发展提出相关的建议。 相似文献
85.
86.
中国北极村气候变暖特征 总被引:2,自引:1,他引:1
利用我国最北部的北极村气象站1963~2005年气温资料,通过计算气候倾向率和气候趋势系数,对该地区气候变化特点进行了分析。结果表明,43年来北极村气温有明显并稳定的上升趋势,年平均气温以每10年0.46℃幅度升高。各季及逐月平均气温都存在不同程度的变暖趋势,但是冬季升温最为剧烈,达每10年0.69℃,其中2月升温幅度为每10年1.02℃,为全年最大。秋季升温最弱,仅为每10年0.21℃。年平均最低气温(每10年0.59℃)和年极端最低气温(每10年0.74℃)比年平均最高气温(每10年0.37℃)和年极端最高气温(每10年0.27℃)升温幅度明显偏大。最低气温比最高气温对平均气温的年代际升温趋势贡献更为明显。 相似文献
87.
88.
89.
Kuranakhite discovered in China for the first time 总被引:4,自引:0,他引:4
Zhou Xinchun Liu Liang Wang Shizhong Wang Yan Yang Jiankun Guo Nenglin Li Guanghui Hu Jianmin 《中国地球化学学报》1998,17(1):77-80
Kuranakhite was firstly discovered in the oxidized zone of the Kuranakh gold mine, southern Russia, and since then there has
been no report on it. Kuranakhite in this paper was discovered in the Jialu gold mine, Luonan County, Shaanxi Province. The
mineral often occurs as irregular granular aggregates varying from 0. 05 to 0. 25 mm in size. The mineral is light brown to
brown in color, translucent, brown in steak, and vitreous in luster. Hv is 231 – 439kg/mm2, HM = 4∼5 and measured density is 6.72(2)g/cm3. Its reflection color is bluishgray to light-blue and it shows middle anisotropism and weak bireflectance. Its polarization
color is blue to grayish-brown and there is no internal reflection. The index of refraction is:N
a = 2.01,N
β = 1. 98,N
γ = 1. 96. The average composition is PbO 45. 40 wt %, MnO2 16.41wt%, TeO3 38.10wt%, totalling 99. 91wt%. The empirical formula is Pb0.99Mn0.92 Te1.06O6, which can be simplified as PbMnTeO6. Principal lines in the X-ray power pattern [d(I)(hkl)] are:0.341 (100), (111); 0.2556(60), (130); 0.2043 (50), (041);0.1666 (20), (310); 0.1598(40), (241); and 0.1472(15), (330).
It was determined that kuranakhite is orthorhombic; its space group may be C;a = 0.511(1) nm,b = 0.891(2)nm,c = 0.532(l)nm, a:b = 0.57, c:b = 0.60;V = 0.242 (3) nm3;Z = 2, and calculated density = 6.66(1) g/ cm3.
This project was financially supported by both the Armed Police Headquarters of Gold Exploration and the Science Foundation
of Shaanxi Provincial Educational Commission (No.HJ96-2-4;96JK-026). 相似文献
90.
Tieguan Wang Dujie Hou Ningning Zhong Jianping Bao Guanghui Huang Linye Zhang Zhilin Chen Peizhen Li 《中国科学D辑(英文版)》1997,40(1):54-64
Taking both eastern Linqing Depression and North Jiangsu Basin as examples, based on geochemical features of immature oils
as well as source inputs of hydrocarbons and macerals, it is revealed that a mixed source input of alga bio-lipids and higher
plant waxes is a basic characteristic of source material for immature oils in non-marine brackish-saline lacustrine basins.
Project supported by the “85–102” Chinese National Key Science and Technology Project and the National Gas Geochemistry Key
Laboratory, Lanzhou Institute of Geology, Chinese Academy of Sciences. 相似文献