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石膏可能成为可燃冰勘探新标志
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《探矿工程》 2003年第3期63-63,共1页
关键词 石膏 可燃冰 勘探标志 天然气水合物 海洋 冻土区 沉积物
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Identification Signs and Prospects of Hydrate Gas
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作者 徐振中 陈世悦 +1 位作者 杨淑卿 马在田 《Marine Science Bulletin》 CAS 2007年第1期84-96,共13页
Gas hydrate is a kind of icy crystal body formed by water and natural gas in special conditions. The discovery of gas hydrates provides a wide sphere and a new way of thinking for finding clean and effective energy re... Gas hydrate is a kind of icy crystal body formed by water and natural gas in special conditions. The discovery of gas hydrates provides a wide sphere and a new way of thinking for finding clean and effective energy resources to replace increasingly exhausted traditional energy resources. Moreover, in our country there are a wide realm and bright prospect in the exploration of gas hydrate. This paper has summarized the progress on the study of gas hydrate. And based on the former research about gas hydrates, the integrative identification signs of gas hydrates were summarized in the aspects of seismic data, geophysical well logging, sedimentary and rock, geochemistry, topography and morphology. In the end, the author hopes it may provide some useful clues to the exploration of gas hydrate. 展开更多
关键词 integrative identification signs gas hydrate exploration
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伊比利亚西南部黄铁矿带中的金成矿
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作者 G.K.Strauss J.S.Beck 彭渤 《国外铀金地质》 1994年第4期306-309,共4页
长期以来,人们对伊比利亚西南部黄铁矿带内古生代火山-沉积环境下块状硫化物矿体中金的产出和分布,看法很不一致。近来对几个正在开采的矿山进行研究表明,矿体的金品位因矿石类型而异,并受沉积期间的物理-化学和时间因素所控制。金品位... 长期以来,人们对伊比利亚西南部黄铁矿带内古生代火山-沉积环境下块状硫化物矿体中金的产出和分布,看法很不一致。近来对几个正在开采的矿山进行研究表明,矿体的金品位因矿石类型而异,并受沉积期间的物理-化学和时间因素所控制。金品位超出平均值的矿石类型有:(1)位于块状硫比物透镜体侧面和顶部的富Pb-Zn矿体;(2)富铜的硅质底部矿石;(3)下盘细脉硫化物;(4)富脉石(硅质基质、富碳酸盐基质、含重晶石基质或含碳基质)块状硫化物。从而提出了对单个矿体的下盘和上盘围岩,以及下盘的浸染状和细脉状矿体进行勘探的可能性。 展开更多
关键词 黄铁矿带 勘探标志 金矿床 矿化 成矿
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Geochemistry of solvable organic matter from source rocks in Shangkuli Formation of Labudalin Basin
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作者 GAO Fuhong GAO Hongmei FAN Fu YANG Yang 《Global Geology》 2010年第2期70-74,共5页
A suit of lacustrine source rocks are developed in volcanic deposits in the Shangkuli Formation of the Cretaceous. However, it is poor to understand the characteristics of source rocks due to the low degree of explora... A suit of lacustrine source rocks are developed in volcanic deposits in the Shangkuli Formation of the Cretaceous. However, it is poor to understand the characteristics of source rocks due to the low degree of exploration, thus the exploration is severely constrained in this area. Based on the geochemical analysis, the analytic technique of GC and GC-MS, combined with the characteristics of solvable organic matter and biomarkers of the source rocks, the authors discussed the depositional environment, the derivation of the matrix and the maturity characteristics of the organic material of the Shangkuli Formation in Cretaceous. The results show that the organic matter mainly belongs to type Ⅱ1 kerogen, whose abundance is relatively high; it was formed in reductive surrounding where was deep-lake; the hydrocarbon is characterized by mixed-source of organic matter. The thermal evolution of source rocks had reached maturation stage. 展开更多
关键词 Labudalin Basin source rocks solvable organic matter
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