中国北方金矿床铅同位素研究

本文着重讨论了我国北方地区几个主要金矿床的形成时代、矿源及其与铅同位素的关系。认为:①从内蒙到东部沿海(包括东北),金矿的形成时代从海西中期(311×10~6a)到燕山晚期(100×10~6a),并且大多数金矿与中生代的岩浆活动有关;②在由岩石铅(包括花岗岩和变质岩)和矿石铅同位素组成的~(207)Pb/~(204)pb-~(208)Pb/~(204)Pb图解上,矿石铅同位素组成更靠近花岗岩一端;③变质岩和花岗岩中的金具有很高的淋洗率,均可作为金矿的矿源岩石。     

黑海清洁计划将于近期实施

由前苏联黑海沿岸国家和土耳其共同制定的对黑海进行清洁的合作计划将于近期付诸实施。由于近几十年来黑海沿岸国家忽视了环境保护工作,致使黑海环境状况日趋恶化,给沿海地区的居民身体健康和经济发展带来严重影响,并严重破坏了周围的自然景观。因此,解     

利用卫星获得全球变暖的资料

来自太空的有关图像可以提供大气中二氧化碳含量方面的资料。随着人们对全球变暖的日益关注,探索海洋对二氧化碳吸收的定量测量方法就显得越来越重要。确定海洋对二氧化碳的吸收有助于解释大气中二氧化碳的平衡问题。在进行光合作用期间,漂浮在海洋上层的单细胞浮游植物吸收二氧化碳,并将二氧化碳     

Clay-mineral suites,sources, and inferred dispersal routes: Southern California continental shelf

Clay mineralogy is useful in determining the distribution, sources, and dispersal routes of fine-grained sediments. In addition, clay minerals, especially smectite, may control the degree to which contaminants are adsorbed by the sediment. We analyzed 250 shelf sediment samples, 24 river-suspended-sediment samples, and 12 river-bed samples for clay-mineral contents in the Southern California Borderland from Point Conception to the Mexico border. In addition, six samples were analyzed from the Palos Verdes Headland in order to characterize the clay minerals contributed to the offshore from that point source. The <2 microm-size fraction was isolated, Mg-saturated, and glycolated before analysis by X-ray diffraction. Semi-quantitative percentages of smectite, illite, and kaolinite plus chlorite were calculated using peak areas and standard weighting factors. Most fine-grained sediment is supplied to the shelf by rivers during major winter storms, especially during El Ni?o years. The largest sediment fluxes to the region are from the Santa Ynez and Santa Clara Rivers, which drain the Transverse Ranges. The mean clay-mineral suite for the entire shelf sediment data set (26% smectite, 50% illite, 24% kaolinite+chlorite) is closely comparable to that for the mean of all the rivers (31% smectite, 49% illite, 20% kaolinite+chlorite), indicating that the main source of shelf fine-grained sediments is the adjacent rivers. However, regional variations do exist and the shelf is divided into four provinces with characteristic clay-mineral suites. The means of the clay-mineral suites of the two southernmost provinces are within analytical error of the mineral suites of adjacent rivers. The next province to the north includes Santa Monica Bay and has a suite of clay minerals derived from mixing of fine-grained sediments from several sources, both from the north and south. The northernmost province clay-mineral suite matches moderately well that of the adjacent rivers, but does indicate some mixing from sources in adjacent provinces.     

储层随机建模方法研究进展

油气储层随机建模方法是近年来新发展起来的一门油气预测技术,它在综合了地质、地球物理信息的基础上,充分利用已知点的储层信息,根据所要预测的储层属性来选择不同的随机模型,从而实现了对油气储层的定量表征及对各种尺度非均质性的定量刻画,其最终模拟结果可以有任意多个以供油藏描述选择。这里简要介绍了目前比较常用的储层随机建模方法、原理,各方法的优缺点,以及不同随机模型的地质适用性,并针对我国储层的特点,指出储层随机建模技术的发展方向。