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101.
滇西北衙金多金属矿床成矿地球化学特征 总被引:10,自引:0,他引:10
北衙金多金属矿床是金沙江-哀牢山-红河断裂带与新生代富碱斑岩有关的斑岩型矿床之一.本文重点提供了流体包裹体中稀土微量元素和矿石S、Pb同位素分析结果,并对成矿流体及成矿物质来源等问题进行了讨论.研究表明,本区流体包裹体稀土总量较低,∑REE介于5.19×10-6~9.0×10-6之间,反映轻重稀土分馏程度的∑LREE/... 相似文献
102.
位于山东烟台的辽上金矿床为一中型金矿,矿床赋存于新元古代玲珑超单元二长花岗岩与古元古代荆山群的接触带附近,发育矽卡岩化,矿体的产出严格受接触带构造控制.区内出露的中生代岩体为石英二长闪长岩.通过研究每个矿体的宏观产出特征,发现金矿体与石英二长闪长岩有关,区域上部分金矿体赋存于石英二长闪长岩中,而与新元古代玲珑超单元二长... 相似文献
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为了探讨玄武岩铜矿成矿流体的特征,对滇黔交界地区峨眉山玄武岩铜矿3个成矿期次铜矿石中石英和方解石的气液包裹体进行了激光拉曼成分研究和均一温度、盐度测定,对古石油包裹体通过荧光显微镜进行了成分鉴定。结果表明:第1、2期次成矿流体主要为盆地卤水,其气液包裹体气液比小(一般5%~10%),w(NaCl)为8%~22%,气相为甲烷,液相为水,无子晶及液相CO2,均一温度为80℃~260℃;第2期次成矿流体除盆地卤水外,还有以古石油为代表的有机流体,古石油包裹体由液态烃、固体沥青和气相组成,均一温度变化大(30℃~290℃),液态烃以荧光性强的芳烃为主;第3期次成矿流体具有大气降水成因,其气液包裹体气液比一般为5%~10%,w(NaCl)〈4%,无子晶及液相CO2,均一温度140℃~270℃,但以小于200℃为主。从第1期次到第3期次,成矿流体盐度逐渐降低,特别是第3期次的盐度非常低,但温度变化不明显。本区最重要的自然铜沉淀富集成矿是第2期次不同性质成矿流体混合或成矿流体与有机流体混合、有机质的还原的结果。 相似文献
106.
山东半岛荆山群富铝片麻岩锆石U-Pb定年及其地质意义 总被引:12,自引:0,他引:12
荆山群富铝片麻岩广泛分布于山东半岛早前寒武纪变质基底之中。锆石阴极发光图像分析和U-Pb定年结果表明,荆山群富铝片麻岩中锆石成因比较复杂,可划分为3种类型:第一类为继承性(岩浆或碎屑)锆石,U-Pb定年结果显示该类锆石微区记录了~2 650 Ma和~2 100 Ma两组207Pb/206Pb年龄,这不仅表明研究区变质基底在中太古代末期和古元古代早期至少存在两期岩浆-热事件,同时,也说明荆山群原岩形成时代应晚于2 100 Ma;第二类为变质锆石,记录的207Pb/206Pb年龄集中在1 900~1 850 Ma之间,应代表荆山群富铝片麻岩峰期高压麻粒岩相变质时代;第三类亦为变质锆石,记录的207Pb/206Pb年龄集中在1 840~1 820 Ma之间,应代表荆山群富铝片麻岩峰后中低压麻粒岩相退变质时代。该项成果准确地限定了荆山群富铝片麻岩的原岩形成时代、峰期高压麻粒岩相变质时代和峰后中低压麻粒岩相退变质时代的年代学格架,对深入探讨华北克拉通东南缘高压麻粒岩的成因机制及其形成的动力学背景具有重要的科学意义。 相似文献
107.
Two Northward Jumps of the Summertime Western Pacific Subtropical High and Their Associations with the Tropical SST Anomalies 总被引:1,自引:0,他引:1 下载免费PDF全文
Based on the pentad mean ridgeline index of the western Pacific subtropical high (WPSH), the authors identified the two northward jumps of the WPSH from 1979 to 2008 and revealed their associations with the tropical SST anomalies. The authors show that the northward jumps, especially the second jump, exhibited remarkable interannual variability. In addition, the authors find that the two northward jumps were mutually independent and were influenced by the SST anomalies in the different regions of the tropical Pacific. The first jump was positively correlated with the SST anomalies in the tropical central Pacific from the preceding winter to June. In contrast, the second jump was positively related to ENSO in the preceding winter, but this correlation tended to weaken with the decay of ENSO and disappeared in July. Instead, a positive correlation was found in the Indian Ocean. We therefore suggest that ENSO plays an indirect role in the second jump through the capacitor effect of the Indian Ocean. 相似文献
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本文以中国西部大地形变监测与地震预测实践为基础, 简要总结回顾了利用大地形变进行强震预测研究的工作思路、方法和一些进展; 进而结合2001年昆仑山口西8.1级、 2008年四川汶川8.0级特大地震前区域地壳运动变形背景和已有的研究结果, 分析和探讨了基于大地形变监测、 并考虑地震构造的差异性来进一步提高大震预测的有效性... 相似文献
110.
Relationship Between the Western Pacific Subtropical High and the Subtropical East Asian Diabatic Heating During South China Heavy Rains in June 2005 下载免费PDF全文
Based on the daily NCEP/NCAR reanalysis data, the position variation of the western Pacific subtropical high (WPSH) in June
2005 and its relation to the diabatic heating in the subtropical East Asia are analyzed using the complete vertical vorticity
equation. The results show that the position variation of the WPSH is indeed associated with the diabatic heating in the subtropical
East Asian areas. In comparison with June climatology, stronger heating on the north side of the WPSH and relatively weak
ITCZ (intertropical convergence zone) convection on the south side of the WPSH occurred in June 2005. Along with the northward
movement of the WPSH, the convective latent heating extended northward from the south side of the WPSH. The heating to the
west of the WPSH was generally greater than that inside the WPSH, and each significant enhancement of the heating field corresponded
to a subsequent westward extension of the WPSH. In the mid troposphere, the vertical variation of heating on the north of
the WPSH was greater than the climatology, which is unfavorable for the northward movement of the WPSH. On the other hand,
the vertical variation of heating south of the WPSH was largely smaller than the climatology, which is favorable for the anomalous
increase of anticyclonic vorticity, leading to the southward retreat of the WPSH. Before the westward extension of the WPSH
in late June 2005, the vertical variation of heating rates to (in) the west (east) of the WPSH was largely higher (lower)
than the climatology, which is in favor of the increase of anticyclonic (cyclonic) vorticity to (in) the west (east) of the
WPSH, inducing the subsequent westward extension of the WPSH. Similar features appeared in the lower troposphere. In a word,
the heating on the north-south, east-west of the WPSH worked together, resulting in the WPSH extending more southward and
westward in June 2005, which is favorable to the maintenance of the rainbelt in South China. 相似文献