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91.
云南兰坪中排李子坪铅锌矿矿床成因 总被引:1,自引:0,他引:1
铅锌矿产于下白垩统景星组下段泥质粉砂岩、钙质砂岩和中侏罗统花开左组上段砂岩夹薄层泥灰岩介壳灰岩中,脉状、透镜状、层状、似层状等产出。NNE向断裂的交叉夹持部位的旁侧派生次级断裂及层间破碎带是主要容矿构造,矿床成因为沉积-中低温热液改造构造控矿型。 相似文献
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In this paper we describe an example of travertine fissure-ridge development along the trace of a normal fault with metre
displacement, located in the eastern margin of the Neogene–Quaternary Siena Basin, in the Terme S. Giovanni area (Rapolano
Terme, Italy). This morphotectonic feature, 250 m long, 30 m wide and 10 m high, formed from supersaturated hot waters (39.9°C)
flowing from thermal springs aligned along the trace of the normal fault dissecting travertines not older than Late Pleistocene
(24 ± 3 ka). A straight, continuous fissure with a maximum width of 20 cm occurs at the top of the ridge, along its crest.
Hot fluids flow from cones mainly located at the extremities of the ridge, where travertine is depositing. The travertine
fissure-ridge shows an asymmetrical profile since it buries the fault scarp. The difference in height of slopes corresponds
to the vertical displacement of the normal fault. Fissuring of the recent travertine deposits along the strike of the crestal
fissure, as well as recent hydrothermal circulation, lead us to believe that the Terme S. Giovanni normal fault may be currently
active. On the whole, the Terme S. Giovanni fissure ridge can be defined as a travertine fault trace fissure-ridge, adding
a helpful example for studying the relationship between faulting and travertine deposition. 相似文献
95.
Christoph Spötl Yuri Dublyansky Michael Meyer Augusto Mangini 《International Journal of Earth Sciences》2009,98(3):665-676
The area south of the prominent east–west trending Salzach Valley at the northern rim of the Central Alps of Austria has long
been known to host anomalously warm springs emerging from a highly deformed calcite marble (Klammkalk). This unit also hosts
cavities whose shapes suggest a hydrothermal karst origin and which are lined by calcite spar. We report here petrographic
and isotopic evidence suggesting that dissolution by ascending low-temperature thermal waters also played an important role
in the origin of a large cave in this region, Entrische Kirche. A paleo cave wall, preserved behind a thick flowstone in the
interior of this cave, revealed a brownish bleaching zone which contrasts to the medium grey colour of the unaltered marble
beneath. Across this zone the C and O isotope values gradually decrease by 3 and 11‰, respectively. These compositions are
very different from those of the speleothem above but are similar to phreatic calcite spar from hydrothermal karst cavities
in other outcrops in the area, where the absence of two-phase fluid inclusions suggests a low-temperature (less than ca. 50°C)
hydrothermal origin. U/Th dating of the flowstone capping the alteration zone yielded a minimum age of the thermal water invasion
in Entrische Kirche of ca. 240 kyr. There is no evidence in Entrische Kirche that these palaeowaters reached the point of
calcite precipitation, but it is physically conceivable that higher and as yet unexplored parts of this deep (ca. 900 m) cave
contain cavities lined by phreatic cave spar. 相似文献
96.
Hg bioaccumulation in marine copepods around hydrothermal vents and the adjacent marine environment in northeastern Taiwan 总被引:1,自引:0,他引:1
The Hg concentration in seawater and copepod samples collected from the area around hydrothermal vents at Kueishan Island and the adjacent marine environment in northeastern Taiwan were analyzed to study Hg bioaccumulation in copepods living in polluted and clean marine environments. The seawater collected from the hydrothermal vent area had an extremely high concentration of dissolved Hg, 50.6–256 ng l−1. There was slightly higher Hg content in the copepods, 0.08–0.88 μg g−1. The dissolved Hg concentration in the hydrothermal vent seawater was two to three orders of magnitude higher than that in the adjacent environment. The bioconcentration factor of the studied copepods ranged within 103–106, and showed higher dissolved concentration as the bioconcentration factor was lower. A substantial abundance, but with less copepod diversity was recorded in the seawater around the hydrothermal vent area. Temora turbinata was the species of opportunity under the hydrothermal vent influence. 相似文献
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99.
安徽池州铜山铜矿床元素地球化学分带特征及意义 总被引:2,自引:1,他引:1
铜山铜矿是长江中下游成矿带内安庆-贵池矿集区中的一个中型矽卡岩型矿床,矿体赋存于铜山岩体与下二叠统栖霞组碳酸盐岩间的接触带内.典型剖面系统取样分析结果显示:从岩浆岩、矽卡岩到碳酸盐岩,元素地球化学组成总体上表现为渐变分带特征,即靠近岩体的矽卡岩富集Si、Fe、Mg及亲铁元素Co和亲铜元素Cu、Ag;远离岩体的矽卡岩富集Ca、Mn、Al、Ti、REE和亲铜元素Pb、Zn;远离大理岩带的强硅化蚀变岩富集Si、Fe、Li和Co,而强烈亏损Ca、Sr和REE.这种分带可以依据元素活化迁移理论加以解释.在矽卡岩形成过程中,岩浆热液携带Si、Fe、Mg、Al、Li、REE、大离子亲石元素Rb、Cs、亲铁亲铜元素Co、V、Zn以及高场强元素Ta、Zr、Nb、Hf、Ga、Be向大理岩迁移并富集于形成的矽卡岩中;大理岩中的Ca被活化后进入矽卡岩体系,而Sr、K及Pb则随流体搬运迁出.蚀变及矿化较弱的矽卡岩稀土总量较高(ΣREE=122.0×10-6),LREE富集[(La/Sm)N =3.99],HREE亏损[(Gd/Yb)N=2.85],Eu显示负异常(δEu =0.69),重稀土配分形式与新鲜石英二长斑岩相似,但La、Ce等轻稀土元素相对亏损.矽卡岩剖面元素分带特征及稀土配分模式指示铜山矽卡岩铜矿床为接触交代成因.结合已有氢氧同位素结果,认为铜山铜矿成矿流体主要来自岩浆热液,在矽卡岩退化蚀变和成矿期间有大气降水混入成矿流体. 相似文献
100.
在新疆西南天山科桑溶洞地区,新厘定出一套斜长角闪岩-花岗岩地质单元:侵入斜长角闪岩中的新元古代白云母花岗岩(片麻状构造)、以及侵入上述古老岩石单元的早奥陶世花岗岩(块状构造)。片麻状白云母花岗岩中锆石具有热液锆石边、岩浆锆石幔和碎屑锆石核(边-幔-核结构),剔除被热液锆石和碎屑锆石混染的SHRIMP测点,获得岩浆锆石幔的加权平均年龄752.3±5.1Ma(MSWD=0.95),代表岩浆的结晶年龄。块状花岗岩的锆石具有边-核结构,热液锆石边的U-Pb年龄(419.5±5.7Ma)明显偏低。剔除热液锆石和碎屑锆石,获得岩浆锆石的平均U-Pb年龄481.1±4.4Ma(MSWD=0.88),代表花岗岩的结晶年龄。早奥陶世早期,岩浆侵入新元古代片麻状白云母花岗岩中。在晚志留世或者更晚时期,两类花岗岩共同经受了变质热液改造,变质流体交代岩浆锆石,导致锆石溶蚀再生长。 相似文献