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61.
Submarine hydrothermal mineralization in the Okinawa Trough, SW of Japan: an overview 总被引:3,自引:0,他引:3
The Okinawa Trough is a heavily sedimented, rifted back-arc basin formed in an intracontinental rift zone. Submarine hydrothermal activity is located within the six back-arc rifts located in the middle and southern Okinawa Trough and its distribution is controlled principally by tectonic factors. Subduction of the Daito and Gagua Ridges beneath the Ryukyu Arc has resulted in fracturing of the brittle lithosphere beneath the Okinawa Trough. Hydrothermal activity is strongest in the volcanic arc-rift migration phenomenon (VAMP) area plus the JADE site and Southernmost Part of the Okinawa Trough (SPOT) area which form the prolongation of these two ridges. These areas are characterized by extremely high heat flow locally. Submarine hydrothermal fluids from the Okinawa Trough tend to be strongly influenced by interaction of the hydrothermal fluids with organic matter in the sediment resulting in high alkalinity and NH4+ concentrations of the fluids. The fluids also contain high concentrations of CO2 of magmatic origin. Submarine hydrothermal mineralization in the trough is diverse. The CLAM site consists principally of carbonate chimneys. Interaction of the hydrothermal fluid with organic matter in the sediment is particularly strong at this site. This is most probably a sediment-hosted deposit in which sulphide minerals have deposited within the sediment column leaving ‘spent ore-fluids’ to emerge at the seafloor. The JADE site consists of active and inactive sulphide–sulphate chimneys and mounds. The Zn–Pb-rich sulphides at this site contain the highest concentrations of Pb, Ag and Au so far recorded in submarine hydrothermal sulphide deposits. At Minami-Ensei Knoll and Hatoma Knoll, active and inactive chimneys consist principally of anhydrite and barite as a result of phase separation of the hydrothermal fluids beneath the seafloor. An intense black smoker has recently been discovered at Yonaguni Knoll in the SPOT area. If it is confirmed that sulphide mineralization is dominant at this site, this could be a highly prospective area. The most prospective areas for economic-grade minerals in the Okinawa Trough appear to be the JADE site and the SPOT area. 相似文献
62.
根据两次资源评价结果的分析和对比,认为值得对古生界进行大规模油气勘探。分析了中国海相油气勘探滞后的原因是地史发展的顺序为先海后陆和海相沉积深度比陆相的大。归纳阐述了适用于海相沉积与陆相沉积的10条基本石油地质认识,指出了我国海相沉积深度大、年代老、生油争议多、气比油多、遭破坏多等特点,建议开展区域地质、碳酸盐岩生油、古隆起带、逆掩断层带、盐下油气、碳酸盐岩储集性、油藏破坏与保存的关系、新技术与新方法等8个方面的研究。 相似文献
63.
64.
世界天然气水合物研究开发现状和前景 总被引:76,自引:1,他引:76
回顾了世界天然气水合物研究历史,分析了世界气水合物研究现状和开发前景,评价了全球天然气水合物资源潜势,提出了我国对天然气水合物的研究策略。 相似文献
65.
重点探讨了与柴达木资源开发相关的五个问题。一是柴达木在青海发展和西部地区资源开发中的地位和作用问题 ;二是格尔木市发展中的几个问题 ,重点探讨了格尔木的城市性质 ,格尔木在国家资源安全中的作用和格尔木进一步发展的问题 ;三是讨论了西部大开发中 ,资源的地位和作用问题 ;四是讨论了投资补偿理论和柴达木盆地矿业城市可持续发展问题 ;最后探讨了柴达木资源综合利用和工业可持续发展问题 相似文献
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67.
This article examines the relationships between foreign direct investment (FDI) and natural resource depletion and natural resource rents for a longitudinal (2005–2013: N?=?125 nations) sample of less developed countries (LDCs). Theoretically, we argue that FDI contributes to increased ecological withdrawals and dependence on the natural resource sector for economic growth within countries. We hypothesized that LDCs with higher levels of FDI would also have higher levels of natural resource depletion and income (i.e., rents). We assess whether this hypothesized relationship holds across nations in our sample for four different natural resource depletion and rents measures (energy, forest, mineral, and total natural resources). We find strong support for our hypotheses regarding natural resource depletion and resource rents, with the exception of energy rents. The outcome lends support to the ecological withdrawal and ecostructural theory of foreign investment dependence perspectives. 相似文献
68.
通过对江苏长江以北地区围岩、岩浆和构造三方面成矿条件分析,提出该区新生界覆盖地区金属矿产成矿潜力大致为:响水—淮阴一线以北浅覆盖地区主要预期类型为斑岩Cu(Au)、Cu-Mo矿床,金山式、焦家式和玲珑式Au矿,此外可能存在不同生的块状硫化物矿床。响水—淮阴一线以南为深覆盖地区,其中埋深在40—500m间的隐伏隆起是现实的找矿目标区,可以预期与宁镇矿集区、铜陵矿集区或利国矿田相类似的各类矿床 相似文献
69.
人口、资源、灾害与环境是困扰当代人类的几个重大问题.人口的增长,要求有更多的资源,而资源开发、利用的合理与否,又势必对环境产生有利或有害的影响;环境的改善或恶化,反过来又必然影响到资源的增减.因此,如何处理好它们之间的关系,使资源得到合理的开发和利用,同时又保护或改善环境,形成资源开发利用与环境保护改善之间的良性循环,应当是人类共同奋斗的一个目标. 本文依据一些实际资料论述了上述问题以及地球物理学在解决这些问题中所应起的作用. 相似文献
70.
Quantitative assessment of mineral resources with an application to petroleum geology 总被引:2,自引:0,他引:2
The probability of occurrence of natural resources, such as petroleum deposits, can be assessed by a combination of multivariate statistical and geostatistical techniques. The area of study is partitioned into regions that are as homogeneous as possible internally while simultaneously as distinct as possible. Fisher's discriminant criterion is used to select geological variables that best distinguish productive from nonproductive localities, based on a sample of previously drilled exploratory wells. On the basis of these geological variables, each wildcat well is assigned to the production class (dry or producer in the two-class case) for which the Mahalanobis' distance from the observation to the class centroid is a minimum. Universal kriging is used to interpolate values of the Mahalanobis' distances to all locations not yet drilled. The probability that an undrilled locality belongs to the productive class can be found, using the kriging estimation variances to assess the probability of misclassification. Finally, Bayes' relationship can be used to determine the probability that an undrilled location will be a discovery, regardless of the production class in which it is placed. The method is illustrated with a study of oil prospects in the Lansing/Kansas City interval of western Kansas, using geological variables derived from well logs. 相似文献