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碳酸盐岩

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Gold occurs mainly in pyrite-sericite-quartz rocks and pyrite±polymetallic-sulphides+quartz±carbonate veins and stockworks, forming veinlet-disseminated ores.

金主要产于黄铁绢英岩和黄铁矿±多金属硫化物+石英±碳酸盐脉-细网脉中,构成细脉-浸染状矿石。

P species, main as Ca-P and organic P forms, showing rego〓 pollution and karst area of lake watershed, inorganic P〓 related to Ca〓, Al〓, Fe〓 content in the overlying water, sediments is not a simple reservoir of dissolved phosphate and particle phosphate, near the interface, near 98% of total P existed as active forms, they may release to overlying water through reduction dissolution, deadsorption in the period of early diagenesis, only 2% of P as fixed forms, which mainly remained in the sediments, sediment was an important resource of nutrients of ovrelying water.

高原湖泊沉积物中的磷以有机磷和Ca-P形式存在为主,反映了高原湖泊流域污染和碳酸盐地区的整体背景,无机磷形式与水体吸附体Ca〓,Al〓和Fe〓的含量有关。底部沉积物不是溶解性磷酸盐和颗粒磷酸盐的长期储存场所,几乎有98%的磷是活性的形态存在,它们通过早期成岩作用在还原条件下还原,溶解和释放又重新回到上覆水体,只有2%的磷以固〓态的形式稳定保存于沉积物中,因此,沉积物为水体营养程度的重要来源。

Most areas in Taiyuan stage are distributed by shallow-sea continental shelf in the southern and eastern part, but in the northern and western part are scattered by clastic tidal flat and carbonate tidal.

太原期研究区南部和东部大部分地区发育浅海陆棚沉积,北部及西部地区则发育碎屑岩潮坪和碳酸盐潮坪。

Shagou vein-type Ag-Pb-Zn ore deposit in the south margin of North China Craton is composed of vein and replacement ore types.

豫西沙沟薄脉状Ag-Pb-Zn硫化物矿床位于华北地台南缘熊耳山地区,由硫化物石英脉和石英-碳酸盐-云母蚀变岩这两种矿化类型组成。

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年美国个人破产法的一个改动使得破产登记急速下降,而后引起了信用卡大规模的亏损。

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