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141.
山东三山岛金矿床流体包裹体特征及其地质意义 总被引:5,自引:0,他引:5
三山岛金矿床位于莱州市三山岛—仓上断裂带内,矿石主要为蚀变岩和含金石英脉2种类型。随着胶东金矿床研究的深入和三山岛金矿资源的不断减少,对三山岛金矿床的成矿作用及深部开发前景问题研究具有更重要的意义。针对上述问题,对三山岛金矿床2种类型矿石的成矿流体特征进行对比研究,认为代表成矿早—中期的蚀变岩型矿石形成于中温(均一温度为325~240℃)、低盐度(2.07%~6.88%)、低密度(0.720~0.868g/cm3)、酸碱性不均匀(pH=3.27~10.43)、以氟化物和氯化物为成矿物质载体的还原性流体;代表成矿中—晚期的含金石英脉型矿石形成于中—低温(均一温度为306~160℃)、低盐度(1.05%~9.73%)、低密度(0.739~0.962g/cm3)、碱性(pH=9.25~9.85)、以氯化物和硫化物为成矿物质载体的还原性流体。成矿流体性质的转变反映了成矿流体处于由比较封闭到比较开放的构造环境的转变期,且成矿流体早期以原生岩浆水为主,后期有变质水、大气降水以及海水的参与作用。三山岛金矿成矿深度为2.5~5km,根据目前的开采深度推算其深部还有一定的资源量可供开发。 相似文献
142.
成都经济区黄壤土壤剖面Pb形态分布特征及其影响因素 总被引:3,自引:1,他引:2
土壤剖面中不同形态铅迁移转化及其影响因素的研究对于了解Pb的土壤地球化学行为具有非常重要的意义。以四川省成都经济区农田生态系统黄壤剖面中不同形态Pb分布特征为例,探讨黄壤剖面中不同形态Pb的迁移转化影响因素及其生态危害性。结果表明:在黄壤剖面中,Pb总量表现为表层富集、深层稳定的特点;弱有机结合态含量表现为表层富集、深层稳定的特点,其他形态Pb含量剖面分布特征不明显;土壤中的Pb主要是以铁锰氧化态和残渣态为主,其他形态Pb含量所占比例较小;成土过程中,随着Pb总量的增加,稳定态Pb含量增加,而活动态相对减少;土壤pH值对各形态Pb含量分布影响较大,尤其是对碳酸盐结合态的影响显著;土壤总有机碳也是影响土壤中各形态Pb含量分布的重要因素之一,尤其是对有机结合态Pb含量影响显著;而随着土壤熟化程度的增加,黄壤剖面中的活动态含量增加,稳定态减少;剖面中的Pb迁移系数和生物可利用系数均较小,说明Pb不易向下迁移,容易在表层富集,对植物及人类有一定的危害。 相似文献
143.
新疆南天山库车坳陷区东秋里塔格断褶带构造特征及新活动性 总被引:2,自引:1,他引:1
库车坳陷是南天山中段新构造运动异常强烈的地区,内部发育有四排近EW向展布的逆断裂-背斜带,由南天山山前向塔里木方向依次为:山麓逆断裂-背斜带;喀桑托开逆断裂-背斜带;秋里塔格逆断裂-背斜带和亚肯盲逆断裂-背斜带.东秋里塔格背斜属秋里塔格逆断裂-背斜带东段部分,其构造运动尤为强烈.研究表明:东秋里塔格背斜是浅部滑脱面与其南翼逆冲断层共同形成的断层传播-滑脱混生褶皱,背斜南翼的浅层逆冲断层和深层的断坡构造是重要孕震场所.东秋里塔格浅部背斜核部的背冲式断裂和北翼的膝折属于派生的次级构造,断裂的规模、错动量有限.东秋里塔格背斜南翼逆断层最新活动错断Ⅱ级阶地砾石层,其活动年代至少为全新世早期,这次错动在地表留有3~4 km长的古地震破裂形迹,说明断裂具粘滑运动特征. 相似文献
144.
新疆与哈萨克斯坦寒武纪磷块岩资源 总被引:1,自引:0,他引:1
新疆和哈萨克斯坦寒武纪均为主要的磷矿成矿时代之一,但所形成的磷块岩资源量差别巨大.新疆寒武纪磷块岩矿层薄、矿石质量差、储量很少,哈萨克斯坦小卡拉套山寒武纪磷块岩矿层厚度大、矿石质量好、储量巨大.从实施“走出去”战略出发,邻国小卡拉套地区丰富的磷矿资源对于弥补新疆磷矿资源的严重不足具有重要意义. 相似文献
145.
146.
LIU Luofu HUO Hong GUO Yongqiang CHEN Lixin LI Shuangwen ZHAO Yande LI Yan WANG Ping CHEN Zhijun 《中国地球化学学报》2008,27(1):1-8
The results presented in this paper indicated that the carbazole-type compounds have high thermal stability and also show stability in oxidation and bio-degradation. This kind of compounds still has high concentrations and a complete distribution in the analyzed dry asphalt samples, showing that they are particularly useful in the study of hydrocarbon migration of the paleo-pools. The difference in the contents of nitrogen compounds in the Silurian dry asphalts from the Awati, Tabei and Tazhong areas is attributed to the difference in the extent of oxidation and (or) bio-degradation for the areas; the Awati and Tabei areas underwent relatively strong oxidation and bio-degradation. During the first stage of hydrocarbon pool formation in the Silurian system in the Tazhong and Tabei areas of the Tarim Basin (at the end of the Silurian period) and at the second stage in the Awati area (in Permian), the hydrocarbons experienced a long-distance migration. 相似文献
147.
Hang Li Dahua Li Tangfu Xiao Libin He Zengping Ning Jialong Sun Changsheng Zhu Yan Shuang 《中国地球化学学报》2008,27(1):21-27
The Jinding Pb-Zn deposit in Yunnan Province is the representative of a Cd-enriched area and mining activities lead to the release of Cd into the hypergenic ecosystem, resulting in Cd pollution. The concentrations of Cd vary greatly from one type to another type of rocks in the mining district. In the host rock, Cd concentrations range from 50×10^-6 to 650×10^-6 with an average of 310×10^-6. In primary ores, Cd concentrations range from 14×10^-6 to 2800×10^-6 with an average of 767×10^-6. However, in oxidized ores, Cd concentrations are highest, varying within the range of 110×10^-6 to 8200×10^-6 , averaging 1661×10^-6. It is shown that the oxidized ores are the main carder and environmental source of Cd. Leaching test showed that Pb/Zn ores are easy to oxidize and thereafter release Cd and other harmful elements. These leached elements in the leachate may be precipitated rapidly in the order of Zn〉Pb〉Cd. As for the concentration distribution of Cd in the Bijiang River, it is estimated to be 15.7 μg/L Cd in water, 49.3 mg/L in suspended substances, and 203.7 mg/L in sediments. The average value of Cd in soil from the polluted area is 83.0 mg/kg. Natural weathering of Cd-rich rocks and minerals imposes a potential environmental risk on the aquatic ecosystem of the Bijiang catchment. 相似文献
148.
Petroleum Migration Direction of the Silurian Paleo-pools in the Tarim Basin, Northwest China 总被引:1,自引:0,他引:1
LIU Luofu ZHAO Ye HUO Hong CHEN Lixin CHEN Yuanzhuang ZHAO Suping LI Chao LI Shuangwen GUO Yongqiang LI Yan 《《地质学报》英文版》2008,82(1):174-183
The results obtained in this paper indicate that carbazole-type compounds have high thermal stability and also show stability in oxidation and bio-degradation. This kind of compounds still has a high concentration and complete distribution in the analyzed dry asphalt samples, showing that they are particularly useful in studying petroleum migration of paleo-pool. During the basin's first-stage of oil-gas pool formation in the Silurian in Tazhong and Tabei areas of Tarim Basin (at the end of Silurian period) and the second-stage in the Awati area (in Permian), the petroleum experienced a long-distance migration. During the formation of the Silurian paleo-pools in Tazhong Uplift at the end of Silurian, the petroleum mainly came from the lower and middle Cambrian source rocks in the Manjiaer sag. The petroleum migrated towards the southwest-south entering the Silurian reservoir beds in Tazhong first. Then, it further migrated within Silurian from northwest to southeast along the highs of the Structural Belts to the region of the Silurian pinchout boundary in Tazhong. In Tabei Uplift, during the first-stage of pool formation, the petroleum was also from the lower and middle Cambrian source rocks in the Manjiaer sag. It migrated northwest entering the Silurian reservoir beds in the Tabei Uplift firstly, and then the migration continued in the same direction within the Silurian reservoirs and finally the petroleum was trapped in higher positions. During the second-stage pool formation in the Silurian beds in the areas around Awati sag, the petroleum mainly came from the lower-middle Cambrian source rocks in the Awati sag. The petroleum migrated from the generation center to Silurian reservoirs in all directions around the sag through major paths, and the petroleum was finally trapped in higher locations. 相似文献
149.
150.