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141.
含油玄武岩中绿泥石的形成温度 总被引:5,自引:0,他引:5
以苏北盆地高邮凹陷闵桥地区含油玄武岩中的绿泥石为研究对象,探讨了其成因和形成温度,认为玄武岩中绿泥石有两种形成方式、五条形成途径:其一为蚀变演化,包括:火山玻璃、斜长石、辉石的蚀变,交代橄榄石斑晶,以及皂石的进一步演化;其二为沉淀结晶,包括从热液中直接沉淀生长和胶体溶液充填后的结晶。计算结果显示,蚀变演化形成的绿泥石,其形成温度为128-271℃;沉淀结晶形成的绿泥石,其形成温度为31-63℃。玄武岩中绿泥石形成温度与埋藏深度间没有明显的线性相关。进一步研究表明,本区玄武岩作为储油层,其进油时的温度为62-118℃,不超出48-137℃。 相似文献
142.
Abstract. The Hishikari epithermal gold deposit consists of the Honko-Sanjin zone and Yamada zone. On the basis of observed crosscutting relationships of veins, vein system in the Hishikari deposit was classified into the early and late veins. They differ from orientation, width, control by unconformity, the amount of displacement and structural features, but have similarity in gold grade and Au/Ag ratios. K-Ar ages are presented for the classified veins to clarify timing of fracturing and duration of mineralization.
Age determination revealed that the early veins in the Honko-Sanjin zone range from 0.86 to 1.11 Ma and that the late veins range from 0.73 to 0. 84 Ma. The economically most important mineralization in the Hishikari deposit occurred around 0.90 Ma in a very short period (about 0.05 million years).
The distribution of mineralization age in the whole Hishikari deposit, occurrences of slickensides and ground water temperatures imply that mineralization lasted longer in the southern part of the deposit. As compared the early veins with late veins, structural changes including width, strike, dip and vein characteristics occurred at around 0.85 Ma. 相似文献
Age determination revealed that the early veins in the Honko-Sanjin zone range from 0.86 to 1.11 Ma and that the late veins range from 0.73 to 0. 84 Ma. The economically most important mineralization in the Hishikari deposit occurred around 0.90 Ma in a very short period (about 0.05 million years).
The distribution of mineralization age in the whole Hishikari deposit, occurrences of slickensides and ground water temperatures imply that mineralization lasted longer in the southern part of the deposit. As compared the early veins with late veins, structural changes including width, strike, dip and vein characteristics occurred at around 0.85 Ma. 相似文献
143.
Abstract: Major and rare earth element contents are reported for Late Archean banded iron formations (BIFs) in the Bababudan Group of the Dharwar Craton, South India. The BIFs are mostly composed of SiO2 (average1ρ = 54.88.1 wt%) and Fe2 O3 * (44.38.2 wt%). The Al2 O3 and TiO2 contents are remarkably low, suggesting that detrital components were starved during the BIF deposition. The BIFs have a LREE-enriched pattern with a relatively high (La/Yb)N (6.644.07). Total REE concentrations (RE) vary from 5.2 to 65.3 ppm. The REE patterns are characterized by the presence of a very large negative Ce anomaly (Ce/Ce*: 0.13-0.83) and a positive Eu anomaly (Eu/Eu*: 0.96-2.45). The Eu/Eu* decreases and (La/Yb)N increases with a increase of RE. These correlations of REE indices are similar to those of modern hydrothermal iron-rich sediments near a mid-ocean ridge (MOR). Greenstones associated with the BIFs have MORB-like geochemical features. These geochemical and geological lines of evidence indicate that the depositional site of the BIFs was remote from a continent and/or island arc and that the BIFs were in situ hydrothermal sediments near a MOR. A striking negative Ce anomaly in the BIFs indicates that oxygenated deep-sea environments emerged at 2.9-2.7 Ga. The existence of contemporaneous Mn deposits in the Dharwar Craton supports this assertion. Our scenario of oxygen in the Earth's surface of the Late Archean is different from long-held notion that the atmosphere and ocean were persistently anoxic throughout the Archean. 相似文献
144.
145.
In the Haushi-Huqf (Eastern Central Oman) as in other parts of the Arabian platform, a major sedimentary break is recorded between the Early Aptian carbonates (Shu'aiba Formation) and the Albian orbitolinid-rich marls (Nahr Umr Formation). The unconformity corresponds to a succession of events: (1) a brusque interruption of the regressive sequence of the Shu'aiba limestone (algae and small rudistid build-ups); (2) a stratigraphic gap related to the Late Aptian; (3) the development of a thick ferruginous crust (hardground) that covered the top surface of the Shu'aiba; the hardground is related to a forced flooding surface; (4) the Shu'aiba was rapidly drowned and buried under the Nahr Umr marls. Moreover, the Shu'aiba limestone was subject to faulting NW–SE-trending normal faults before lithification and formation of the ferruginous crust. The faulting episode is clearly dated: post-Early Aptian and pre-Albian. The signification of the faulting remains hypothetical. The syndiagenetic NW–SE normal faults may correspond to ‘en echelon’ faults, combined with transcurrent fault movements (for example the Haushi-Nafun Fault). The possible causes of these intra-platform transcurrent movements are discussed. To cite this article: C. Montenat, P. Barrier, C. R. Geoscience 334 (2002) 781–787. 相似文献
146.
Straight river is generally regarded as one of the typical river patterns in conventional classifications in terms of their channel plain landforms. However, very few straight patterns were found to be distributed in wider spatial and temporal spans in the self-adjusted fluvial rivers. Thus, the questions occur such as that is it possible for a channel takes on a stable straight pattern? What are the main factors controlling the processes of the river pattern formation and transformation from a straight to other patterns? Various theories and hypotheses including geomorphic threshold hypothesis, the extreme hypothesis on energy dissipation rate, the stability theory, etc. have been developed to explain the aforementioned questions, but none of them is sound for the explanation to the straight-river formation. From the modern fluvial plain patterns, the straight patterns are not as stable as other typical patterns which occurred in nature; from the historic records of the river sedimentation, no apparent evidence was found to support the stable straight river evolution. Based on the analysis of existing theories, observations, evolvement processes of the channel patterns in the experimental results, this paper concluded that the straight pattern should not be included as one of the typical patterns that are self-formed and developed. This study is of importance to understanding of the river pattern formation and transformation. 相似文献
147.
148.
塔里木盆地地貌过程对绿洲形成演变的影响 总被引:2,自引:5,他引:2
第三纪末以来,天山、昆仑山强烈隆起使塔里木盆地相对下沉,山盆高差悬殊大,白山顶至盆地腹部地貌外力作用过程依次由冰川作用→冰缘作用→流水作用→干燥作用→冲→洪积作用→湖积作用→风沙作用过渡。在山区河谷平原、平原区冲积扇、冲积平原、湖积平原等地方形成条带状、串珠状、扇形状绿洲,绿洲平面几何形状与适宜绿洲形成与发展的地貌类型空间分布基本吻合。绿洲荒漠化和荒漠绿洲化与地貌过程的关系密切。纵观区内地貌过程发展趋势可预测,区内流水、风沙和人类活动三大地貌过程将有增无减,流水侵蚀与风蚀风积作用将对绿洲产生不良作用。山区流水侵蚀过程加强导致山麓地带绿洲山洪泥石流危害加重。平原河流下游地区流水作用减弱,风蚀风积过程加剧,由绿洲→荒漠演变,而人类活动可分建设作用与破坏作用两方面,前者可稳定绿洲乃至促进荒漠绿洲化而后者则导致绿洲荒漠化。因此,改善山区、山麓地带,特别是盆地南缘与塔河中、下游等重要地区地貌过程并防止绿洲荒漠化,是保障区域可持续发展的有效途径。 相似文献
149.
结合许家湾滑坡灾害点的地质背景资料和现场勘察结果,从滑坡区的地貌、区域地质构造、地层岩性、土壤特性、水文地质特征以及人类工程活动等方面分析滑坡成因机制。指出同向多层次结构的边坡类型、山高坡陡及地表水汇集走廊的地貌特征、发育多组密集节理的区域地质构造、软硬互层的地层岩性、土体的残余强度特性等是滑坡形成的内因;而人为削坡、强降雨和破坏植被营造水耕梯田等人类活动所造成的流水浸蚀,是滑坡形成的诱发空子。基于滑坡稳定性的定量计算,确定了采用抗滑挡土墙、格构式地梁和垫梁组成抗滑系统,并布置了由树枝笼渗沟构成的排水系统等工程治理措施。现场监测结果表明滑坡治理措施卓有成效。 相似文献
150.