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241.
242.
新疆哈密维权银(铜)矿床地质特征和成矿时代 总被引:18,自引:2,他引:18
维权银(铜)矿床是2000年发现的一个独立中型银矿。经过野外及室内研究,发现矿床产于塔里木板块北缘活动带觉罗塔格晚古生代岛弧带的南侧,赋矿地层为中石炭统土古土布拉克组浅海相中酸性、基性火山岩、碎屑岩和碳酸盐岩,受区域早期热蚀变作用而发生不含矿的角岩化;受晚期岩体侵入活动作用形成Ag、Cu等矽卡岩矿化;容矿岩石为钙铁榴石矽卡岩,是一个远离侵入体的以银为主的多金属矽卡岩型矿床。采集维权银(铜)矿东南部花岗岩进行单颗粒锆石的SHRIMPU_Pb年龄测定,结果为(297±3)Ma,是矿床成矿年龄的上限。 相似文献
243.
博斯腾湖湖泊沉积物光释光年代测量* 总被引:2,自引:0,他引:2
使用光释光年代学的单片再生法测量了博斯腾湖沉积剖面中碳酸盐泥及粉砂质泥底部的浅湖相灰色粉细砂和风成沙的年龄,对剖面上部碳酸盐层中陆生植物残体进行了AMS 14 C测年。通过不同测片的等效剂量(De)值的分布状况评价了样品的晒褪程度,选择不随灵敏度校正后的自然释光信号变化的相对集中的等效剂量(De)值计算了样品的埋藏年龄。通过这些年龄结果的对比,发现石英矿物的OSL年龄和AMS 14 C年龄在地层上是一致的,表明尽管在浅湖相细砂中存在不完全晒褪,但根据相对较小而集中的De值计算得到的年龄结果是可靠的。这些年龄结果和地层资料揭示末次冰消期以来至早全新世,博斯腾湖处于无水干盆地向深水湖泊转化的浅水湖泊状态,现代深水博斯腾湖大约形成于距今8ka前后。 相似文献
244.
The Otranto–Leuca coastal tract is marked by the presence of numerous sea caves placed close to present sea level. They are located generally at the back of a shore platform covered by a sequence of breccia deposits, marine sediments and speleothems. At Grotta di Masseria dell'Orte, marine cemented sands rest on a narrow shore platform at about 6.2 m above mean sea level and are covered by speleothems older than 185 ka. At Grotta del Diavolo, which is mostly filled by breccia deposits, three beach levels have been detected at about 3.0, 3.5 and 5.9 m above msl. They are either covered by or overlie speleothems that yield an U/Th age of 340, 78 ka and between 170.3 and 146.5, respectively. Geomorphological evidence and radiometric ages indicate that the area after a period of uplift has been tectonically stable since the last part of the Middle Pleistocene so that marine landforms close to the present shoreline underwent a polycyclic evolution. The sedimentary fills of sea caves formed during Middle-Late Pleistocene glacial stages, when arid or semiarid conditions promoted the removal of regolith and the development of thick breccia deposits. During Marine Isotope Stages (MIS) 9.3, 5.5 and 5.1, cave sediments were partially eroded whereas beach layers and related speleothems developed. These are, in fact, the only marine isotope stages marked by a sea level position which in this Mediterranean region was either close to, or slightly higher than, the present one. 相似文献
245.
In marine strata from Sinian to Middle Triassic in South China, there develop four sets of regional and six sets of local
source rocks, and ten sets of reservoir rocks. The occurrence of four main formation periods in association with five main
reconstruction periods, results in a secondary origin for the most marine gas pools in South China. To improve the understanding
of marine gas pools in South China with severely deformed geological background, the dominant control factors are discussed
in this paper. The fluid sources, including the gas cracked from crude oil, the gas dissolved in water, the gas of inorganic
origin, hydrocarbons generated during the second phase, and the mixed pool fluid source, were the most significant control
factors of the types and the development stage of pools. The period of the pool formation and the reconstruction controlled
the pool evolution and the distribution on a regional scale. Owing to the multiple periods of the pool formation and the reconstruction,
the distribution of marine gas pools was complex both in space and in time, and the gas in the pools is heterogeneous. Pool
elements, such as preservation conditions, traps and migration paths, and reservoir rocks and facies, also served as important
control factors to marine gas pools in South China. Especially, the preservation conditions played a key role in maintaining
marine oil and gas accumulations on a regional or local scale. According to several dominant control factors of a pool, the
pool-controlling model can be constructed. As an example, the pool-controlling model of Sinian gas pool in Weiyuan gas field
in Sichuan basin was summed up. 相似文献
246.
Environmental tracers are used to estimate groundwater ages and travel times, but the strongly heterogeneous nature of many subsurface environments can cause mixing between waters of highly disparate ages, adding additional complexity to the age-estimation process. Mixing may be exacerbated by the presence of wells because long open intervals or long screens with openings at multiple depths can transport water and solutes rapidly over a large vertical distance. The effect of intraborehole flow on groundwater age was examined numerically using direct age transport simulation coupled with the Multi-Node Well Package of MODFLOW. Ages in a homogeneous, anisotropic aquifer reached a predevelopment steady state possessing strong depth dependence. A nonpumping multi-node well was then introduced in one of three locations within the system. In all three cases, vertical transport along the well resulted in substantial changes in age distributions within the system. After a pumping well was added near the nonpumping multi-node well, ages were further perturbed by a flow reversal in the nonpumping multi-node well. Results indicated that intraborehole flow can substantially alter groundwater ages, but the effects are highly dependent on local or regional flow conditions and may change with time. 相似文献
247.
Geographies of age: thinking relationally 总被引:1,自引:0,他引:1
In contrast to recent treatment of other social identities, geographers' work on age still focuses disproportionately on the social-chronological margins – the very young and (to a far lesser extent) the very old – and rarely connects them directly. We outline the benefits of creating relational geographies of age, in order to build out from the recent explosion of children's geographies, and discuss three helpful concepts: intergenerationality, intersectionality and lifecourse. We suggest that participation provides one epistemological vehicle for getting beyond geographies which are mainly adults'. 相似文献
248.
南方海相地震资料脊波非线性阈值去噪方法 总被引:2,自引:0,他引:2
小波分析方法在数据处理中已得到成功广泛的应用,这主要得益于它的局部时频分析能力,但是小波分析对方向的表征能力有限。脊波变换具备优越的方向选择性能,能更好地处理含有线状变化特征的信号。本文针对低信噪比地震记录,尝试研究利用脊波变换方法对其进行处理,提高剖面资料信噪比,突出同相轴信息。在对南方某油田的实际地震资料的处理中,可以发现处理后的地震剖面同相轴品质及连续性有了明显改善,信噪比增强,分辨率相应提高,体现出了该方法相对常规小波分析方法的优越性。 相似文献
249.
Abstract The age of the Yokawa Formation of the Cenozoic Kobe Group distributed in Hyogo Prefecture of western Japan based on mammalian fossils is discussed. Two fossil dental specimens of terrestrial mammals discovered from the lowest part of the Yokawa Formation in the Sanda area are described. These two fossils described here are: (i) a right mandibular fragment with p2–m3 of Bothriodon sandaensis sp. nov. (selenodont anthracotheriid artiodactyl), which appears to be the most primitive among the species of the genus; and (ii) right m1–m3 of cf. Hyrachyus sp. (primitive rhinocerotoid perissodactyl). In the lower part of the Yokawa Formation, Zaisanamynodon (amynodontid perissodactyl) was previously reported. The morphology ('evolutionary stage') of B. sandaensis is indicative of the latest Middle to Late Eocene, that of cf. Hyrachyus sp. is indicative of the Early to Middle Eocene, and Zaisanamynodon is indicative of the Late Middle to Late Eocene. Therefore, the fossil mammals of the Yokawa Formation indicate an latest Middle Eocene ( ca . 38 Ma) correlation for the lower part of the formation, as a working hypothesis. Although the resolution of the geological age based on these mammalian fossils is relatively low compared to that based on marine index fossils, this result is concordant with the recent radiometric correlation of the lower part of the Yokawa Formation in the Sanda area. 相似文献
250.