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121.
Wang Yong Hou Zengqian Mo Xuanxue Dong Fangliu Bi Xianmei Zeng Pusheng 《Frontiers of Earth Science》2007,1(3):322-332
More than 140 middle-small sized deposits or minerals are present in the Weishan-Yongping ore concentration area which is
located in the southern part of a typical Lanping strike-slip and pull-apart basin. It has plenty of mineral resources derived
from the collision between the Indian and Asian plates. The ore-forming fluid system in the Weishan-Yongping ore concentration
area can be divided into two subsystems, namely, the Zijinshan subsystem and Gonglang arc subsystem. The ore-forming fluids
of Cu, Co deposits in the Gonglang arc fluid subsystem have δD values between −83.8‰ and −69‰, δ18O values between 4.17‰ and 10.45‰, and δ13C values between −13.6‰ and 3.7‰, suggesting that the ore-forming fluids of Cu, Co deposits were derived mainly from magmatic
water and partly from formation water. The ore-forming fluids of Au, Pb, Zn, Fe deposits in the Zijinshan subsystem have δD
values between −117.4‰ and −76‰, δ18O values between 5.32‰ and 9.56‰, and Δ13C values between −10.07‰ and −1.5‰. The ore-forming fluids of Sb deposits have δD values between −95‰ and −78‰, δ18O values between 4.5‰ and 32.3‰, and Δ13C values between −26.4‰ and −1.9‰. Hence, the ore-forming fluids of the Zijinshan subsystem must have been derived mainly
from formation water and partly from magmatic water. Affected by the collision between the Indian and Asian plates, ore-forming
fluids in Weishan-Yongping basin migrated considerably from southwest to northeast. At first, the Gonglang arc subsystem with
high temperature and high salinity was formed. With the development of the ore-forming fluids, the Zijinshan subsystem with
lower temperature and lower salinity was subsequently formed.
Translated from Mineral Deposits, 2006, 25(1): 60–70 [译自: 矿床地质] 相似文献
122.
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125.
萨拉乌苏河流域150 ka BP以来的粒度旋回 总被引:18,自引:1,他引:18
萨拉乌苏河流域米浪沟湾地层剖面150kaBP以来古流动砂丘砂与河湖相和古土壤在粒度上具有多次显著的粗细韵律交替变化,粒度参数-Mz、σ、Sk、Kg和SC/D亦随之响应为多波动峰谷交替的态势,同时,粒度特征值-φ5、φ16φ、φ25、φ50、φ84、φ9相应地表现为非常有节奏地跳动,据此,将米浪沟湾剖面划分为27个粒度粗细沉积旋回,并认为其是150kaBP以来在东亚冬夏古代季风交替影响下沙漠演变的一个颇为完整的气候-地质过程记录。 相似文献
126.
Twenty-two peat samples collected at different depths of a core including the layer affected by the 1908 explosion in Tunguska
area of Central Siberia, Russia, and three basalt samples collected near the site, are analyzed by ICP-MS. The concentrations
of Pd, Ni, Co, ΣREE, Ti and Sr in the event layers are 4–35 times higher than the background values in the normal layers.
The variation of Pd is closely related to Ni, Co and ΣREE in the event layers, but not to these elements in the normal layers.
It indicates that these excess elements came from the same source, i.e. the Tunguska explosion body. In addition, the patterns
of Cl-chondrite-normalized REE in the event layers ((La/Yb)N ≈2–3) are much flatter than those in the normal layers ((La/Yb)N ≈7–143), and differ from those in the three basalt samples. The concentrations of REE in the three basalt samples are tens
times higher than those in the event layers. It may be inferred that these excess elements could not be produced by the contamination
of the terrestrial material, but probably by the Tunguska explosion body. Additionally, the ratios of Ti/Ni and Sr/Co in the
event layers are close to those in comet. It implies that the solid part of the explosion body was compositionally similar
to carbonaceous chondrites (Cl) and more probably a small comet. In terms of the Pd excess fluxes in the explosion area, it
can be estimated that the celestial body that exploded over Tunguska in 1908 weighed more than 107 tons, corresponding to a radius of > 126 m. 相似文献
127.
八家子银多金融矿矿田成矿规律与成矿预测 总被引:3,自引:0,他引:3
八家子矿田由NW、NE向两组断裂带与孤形推覆构造交织,控制构成银铅锌、银铁矿床成矿系列,基成矿组份具有组合分带特征。预测东山-冰沟银、铅、锌、炉沟钼和冰沟里银多金属找矿区,经验证,获得找矿成效。 相似文献
128.
随机地震动场激励下拱坝多点输入的抗震可靠度分析 总被引:5,自引:3,他引:5
本文首次将空间随机地震场输入用于拱坝随机振动分析之中,与拱坝三维动力学有限元法结合,完成了三维拱坝在空间随机地震动场作用下的随机振动分析方法及算法的研究,另外考虑动力和静力的叠加,提出了三维空间随机地震动场的拱坝抗震可靠度分析方法,最后编制了相应的程序,对小湾拱坝进行了抗震可靠度分析,并与随机变量的结果进行了比较。 相似文献
129.
交城断裂中段的活动特征及其地震危险性 总被引:8,自引:0,他引:8
通过野外调查和对地质资料、地震活动性资料的综合分析,把交城断裂中段进一步划分为南亚段和北亚段。指出断裂南亚段存在发生6.8级地震的危险性 相似文献
130.