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101.
102.
PENGRunmin ZHAIYusheng 《《地质学报》英文版》2004,78(2):534-547
Most ore-forming characteristics of the Langshan-Zha‘ertaishan hydrothermal exhalation belt, which consists of the Dongshengmiao, Huogeqi, Tanyaokou and Jiashengpan large-superlarge Zn-Pb-Cu-Fe sulfide deposits, are most similar to those of Mesoproterozoic SEDEX-type provinces of the world. The characteristics include: (1) All deposits of this type in the belt occur in third-order fault-basins in the Langshan-Zha‘ertaishan aulacogen along the northern margin of the North China Platform; (2) these deposits with all their orebodies hosted in the Mesoproterozoic impure dolomite-marble and carbonaceous phyllite (or schists) have an apparent stratabound nature; ores display laminated and banded structures, showing clear depositional features; (3) there is some evidence of syn-sedimentary faulting, which to a certain extent accounts for the temporal and spatial distribution and the size of the orebodies in all deposits and the formation of intrabed conglomerates and breccias; (4) they show lateral and vertical zonation of sulfides; (5) The Cu/(Pb Zn Cu) ratio of the large and thick Pb Zn Cu orebodies gradually decreases from bottom to top; and (6) barite is interbedded with pyrites and sometimes with sphalerite. However, some characteristics such as the Co/Ni radio of the pyrites, the volcanism, for example, of the Langshan-Zha‘ertalshan metallogenic belt, are different from those of the typical SEDEX deposits of the world. The meta-basic volcanic rock in Huogeqi, the sodic bimodal volcanic rocks in the Dongshengmiao and potassic bimodal-volcanic rocks with blastoporphyfitic and blasto-glomeroporphyritic texture as well as blasto-amygdaloidal structure in the Tanyaokou deposits have been discovered in the only ore-bearing second formation of the Langshan Group in the past 10 years. The metallogeny of some deposits hosted in the Langshan Group is closely related to syn-sedimentary volcanism based on the following facts: most of the lead isotopes in sphalerite, galena, pyrite, pyrrhotite and chalcopyrite plot on both sides of the line for the mantle or between the lines for the mantle and lower crust in the lead isotope composition diagram; cobalt content of some pyrites samples is much higher than the nickel content (Co/Ni= 11.91-12.19). Some volcanic blocks and debris have been picked out from some pyritic and pyrrhotitic ores. All Zn-Pb-Cu-Fe sulfide orebodies in these deposits occur in the strata overlying metamorphic volcanic rocks in the only ore-bearing second formation. In the Jiashengpan deposit that lacks syn-sedimentary volcanic rocks in the host succession only Pb and Zn ores occur without Cu ore, but in the Dongshengmiao, Tanyaokou and Huogeqi deposits with syn-sedimentary volcanic rocks in the host succession Cu ores occur. This indicates a relatively higher ore-forming temperature. The process of synsedimentary volcanic eruption directly supplied some ore-forming elements, and resulted in secular geothermal anomaly favorable for the circulation of a submarine convective hydrothermal system, which accounts for the precipitation of deep mineralizing fluids exhaling into anoxidic basins along the syn-sedimentary fault system in the Langshan-Zha‘ertai rift. The Dongshengmiao, Tanyaokou, and Huogeqi deposits hosted in the Langshan Group appear to be a transitional type of mineral deposit between SEDEX and VMS-types but with a bias towards SEDEX, while the Jiashengpan deposit hosted in the Zha‘ertai Group is of a characteristic SEDEX type. This evidence, together with other new discoveries of Mesoproterozoic volcanic rocks and the features of lithogeny and metallogeny of the Bayun Obo deposit in the neighborhood emphasize the diversity, complexity and uniqueness of the Mesoproterozoic Langshan-Zha‘ertal-Bayun Obo ore belt. 相似文献
103.
104.
洛川黄土剖面中矿物固定态铵的分布 总被引:1,自引:2,他引:1
对洛川黄土中的固定铵进行了初步分析。结果表明,在所测定的黄土古土壤层中,固定铵态氮含量在130-1之间变化。黄土中的固定铵态氮含量明显低于古土壤。13万a以来洛川黄土剖面中固定铵的分布呈~210现三次大的低高值的振荡特征,即末次间冰期S1古土壤中固定铵态氮含量最高,其次为冰后期的S0古土壤层,末次冰期形成的马兰黄土中固定铵态氮含量最低;在马兰黄土中同样体现出三次小的低高值的波动特征。黄土与μm组分的分布具有相似性,这些特征反映了洛川黄土中固定铵态氮的含量变化与气互层的古土壤中固定态铵的分布与黄土高原区气候的冷暖变化有较好的一致性,并且13万a以来洛川黄土剖面中固定铵的分布与磁化率和<2候条件有紧密的联系,揭示了黄土中固定铵的变化在一定程度上能指示黄土高原区古气候的演变。 相似文献
105.
Xiang-ChuYin Huai-ZhongYu V.Kukshenko Zhao-YongXu ZhishenWU MinLi KeyinPeng S.Elizarov QiLi张晖辉 颜玉定尹祥础 《世界地震译丛》2005,(2):36-43
为了验证大地震发生前或者非均匀脆性介质宏观破坏前加卸载响应比和能量加速释放等前兆现象,本文进行了三轴应力(压缩)条件下大尺度岩石破坏声发射实验。实验采用4组岩石试件,并且分为单调加载和循环加载两种方式。实验结果证明了脆性材料宏观破坏前加卸载响应比升高和能量加速释放这两种前兆现象。本文提出了一种描述岩石试件损伤演化的新的物理量——态矢量。 相似文献
106.
Water soluble components of PM10 Chongqing, China 总被引:1,自引:0,他引:1
The concentrations of water soluble ions (Na+, NH4
+, K+, Mg2+, Ca2+, NO3
-, Cl-, and SO
4
2-
) in PM10 samples collected on cellulose filters by a medium-volume cascade impactor were determined, which were obtained from three
kinds of areas in Chongqing: industrial area (Jiulongpo district), commercial and residential area (Jiangbei district) and
background area (Jinyun Mountain in the Beibei district). The results showed that except for the background site, the annual
average values of PM10 are 23% – 61% higher than the national air quality standard (GradeII) (0.1 mg/m3), even that the value of the control site is still 20% higher than American standard (0.05 mg/m3). This implied that serious pollution of fine particles occurred in Chongqing. Nine kinds of soluble ions in water of PM10 were analyzed by ion chromatography (IC) and the annual average concentrations follow the order of [SO
4
2-
] > [NO3
-] > [Cl-] > [F-], and [Ca2+] > [NH4
+] > [K+] > [Na+] > [Mg2+]. Their values were different in these areas: the industrial area > the commercial and living area > the control area. As
for NH4
+, K+, Ca2+, NO3
- and SO
4
2-
, their seasonal average concentrations show a similar variation trend: the values in spring and fall were higher than those
in summer and winter. The seasonal average concentrations of [Cl-], [F-], [Na+] and [Mg2+] are much lower than those of other ions. However, the concentrations of [Na+] changed more greatly in different seasons than those of the other three ions. Correlation coefficients showed that the three
areas have been polluted by coal smoke and dust to different extents, while some local resources of pollution should be taken
into consideration as well. 相似文献
107.
常规化探方法勘查砂岩型铀矿难以奏效.应用深穿透地球化学方法系列中的元素活动态测量法在鄂尔多斯盆地砂岩型铀矿上的试验结果表明,几种U元素活动态在矿体上方都有异常出现,特别是其中的粘土吸附态U含量级别高、异常衬度大.因此,土壤粘土吸附态U测量法是本区化探找铀矿的有效方法;取样深度和取样粒级分别以60~90 cm和-120目为宜;采用400m的取样点距基本不影响本区砂岩型铀矿的找矿效果.在盆地东北部应用土壤粘土吸附态U测量法预测了3个有利地段,并在其中1个地段的深部发现了较好的铀矿化. 相似文献
108.
北京市不同土地利用类型的土壤砷含量特征 总被引:42,自引:4,他引:42
通过对北京市菜地、稻田、果园、绿化地、麦地以及自然土壤6种土地利用类型共500 个土壤样品的调查分析,探讨了不同土地利用方式对土壤砷积累的影响。与北京市土壤背景值相比,砷在土壤中均有不同程度的增加,累积现象比较普遍。在6种土地利用类型中,自然土壤的砷含量最低,最接近背景值;菜地和稻田的土壤砷含量的增加最为显著。以基线值为标准,北京市涉及土地利用的土壤砷含量总体超标率为1.8%;6种土地利用类型中,菜地、果园、麦地三种土壤砷含量的超标率分别为2.6%、2.7%、0.7%。土壤砷含量的平均值由高到低分别为:稻田>绿化地>菜地>果园>麦地>自然土壤。 相似文献
109.
110.
文章选择鹿回头近岸海域常见的板叶角蜂巢珊瑚(Favites complanata)和十字牡丹珊瑚(Pavona decussata)为研究对象, 采用室内连续培养的方法, 探究两种不同造礁石珊瑚对酸化和溶解有机碳(DOC)加富的响应。结果表明: 酸化(pH 7.6)并不会影响两种珊瑚的钙化速率和生长速率; 但DOC加富(524.03±78.42μmol•L-1)使两种珊瑚的钙化速率分别降低67%和47%、生长速率降低59%和40%。当二者共同作用时, 两种珊瑚的钙化速率降低30%和11%、生长速率降低46%和59%, 大多没有DOC单独作用时强烈, 表现出一定的拮抗作用。两种珊瑚共生虫黄藻叶绿素荧光指数(Fv/Fm)均升高后降低, 板叶角蜂巢珊瑚Fv/Fm最先降低。实验表明, 这两种珊瑚虽然对海洋酸化的敏感度不高, 但是对有机物加富有不同的响应, 板叶角蜂巢珊瑚更为敏感, 可能导致这两种珊瑚在未来环境变化中有不同命运。 相似文献