Developmental modes of the Neoproterozoic-Lower Paleozoic marine hydrocarbon source rocks in China

Based on the researches on rock type, the mode of occurrence, diagnostic minerals and creatures, the sedimentary geochemistry and organic facies of Chinese marine source rocks from wells and outcrops, and on the research findings of developmental modes of foreign marine source rock, the authors consider that it is impossible to objectively make clear the formation mechanism of hydrocarbon source rock with high organic matter abundance by either single mode of preservation or high organic matter productivity. According to the Chinese geological features, the formation mechanism of the Neoproterozoic-Lower Paleozoic marine source rock is generalized into four modes, namely, thermal water activity-upwelling flow-anoxic; carbonate gentle slope-upwelling flow; xerothermic climate-brine euxinic milieu; and humid climate-retained euxinic milieu; as the Lower Cambrian undercompensation basin organic facies （the Tarim Basin, South China and southwestern margin of North China）, carbonate gentle lime mud bound organic facies （the Upper Ordovician in Tazhong region of the Tarim Basin and the Lower Silurian in the Upper Yangtze Platform）, the Middle Cambrian evaporation laggon organic facies （the Tarim Basin and the Upper Yangtze Platform）, enclosed undercompensation terrigenous bay organic facies （the Middle-Upper Ordovician in the west of the Tarim Basin, the Lower Silurian Long- maxi Formation in the Upper Yangtze platform）. Chinese marine sedimentations with lower organic matter abundance are generalized into two modes of consumption-dilution mode of open epicontinental sea and depletion-dilution mode of supercompensation basin.     

浅谈挖掘机的使用

挖掘机是土石方工程施工的主要机械之一，能在坚实的土壤和爆破后的岩石中进行挖掘作业，还可以更换各种工作装置，在建筑工程施工中得到广泛的应用，为提高挖掘机的使用效率就要注意挖掘机的正确使用。     

“诺亚洪水”之谜

在世界各地的古老民族中几乎都有关于史前大洪水的传说,其中最为著名的当属“诺亚洪水”。那么,像“诺亚洪水”那样     

月球上的岩石

千百年来,嫦娥奔月的神话一直鼓舞着我们民族,去攀登天上那个神奇陌生的世界.改革开放的成功,使我们具备了实现这个梦想的实力.最近英国观察家评论说,只要中国人愿意,他们有能力在10～12年内实现载人登月飞行!     

石油百科知识：综合录井（二）

岩屑录井 是获取井下地层岩石样品的重要手段。录井时，要随钻井进尺每隔1米左右从返出的钻井液中捞取一包砂样，并洗净晒干，进行岩性观察描述，并挑选出相对应地层的岩样。因砂样中混有上部地层的岩屑，通常是根据砂样中不同岩样的百分含量和最新出现的岩屑成分来确定岩性，并用钻时快慢区分砂岩、泥岩等。若是发现钻时快，     

谈我国石材开发与研究工作

我国有丰富的石材资源,遍布全国二十余省,现在还缺乏详细的勘探统计资料,据四十多个矿区的调查,储量在240亿立方米以上。意大利虽号称“世界大理石王国”,但是他们的花岗石荒材大都是从国外进口的,所以从资源来说,我国有极大的优势。随着生产的发展,人们对美化建筑及各种工程的要求提高了,饰面板、地板、卫生间设施、工艺品及雕像等多采用大理石或花岗石制作,其需要量越来越大。近年,我国为修建高级宾馆、商场等向国外购进大批高档石材,花费很多外汇。国内若能大批生产这些石村,其社会和经济效益将是很可观的。石材的应用以板材为主要产品,…     

基于生成对抗网络的砂岩薄片图像视野外重建

利用生成对抗网络(GAN)模型,对砂岩薄片图像的微观颗粒和孔隙结构进行视野外重建,并对预测图像的语义进行评价。结果表明,模型能够预测2.25倍于原始视野的砂岩微观结构,并且针对不同类型的岩石图像语义均具有良好的性能。模型对不同颗粒的表面纹理、颗粒形态以及多颗粒间复杂接触关系等语义的图像视野外预测结果与真实图像较为吻合。但是,在微观特殊现象图像的视野外重建任务中,模型缺乏对特殊现象的敏感性。在孔隙结构重建时,模型对微孔面孔率的预测误差大于粒间孔、裂隙和溶蚀孔等孔隙空间。不同孔隙空间重建图像的预测效果可能与孔隙特征(如孔径大小和连通性)有关。     

甘肃省的饲料矿产及开发

介绍了国内外饲料矿产的研究应用现状。在野外调查和室内综合分析的基础上,详细叙述了甘肃省饲料矿产的种类、分布和开采条件,依据饲料矿产的评价原则,论述了甘肃省饲料矿产的开发应用前景。     

新疆东昆仑阿其克湖蛇绿岩的确定——来自岩石地球化学研究的证据

岩石地球化学研究结果证明,出露在新疆东昆仑阿其克湖西南畔的一套超镁铁-镁铁岩组合属于上俯冲带(SSZ)型蛇绿岩的一部分,可能形成于弧前或弧后盆地,文中将其称为"阿其克湖蛇绿岩".根据区域地质调查资料和同位素年代学的研究结果,认为该蛇绿岩可能形成于前泥盆纪,区域上出露的晚古生代浅海相沉积地层不整合覆盖在其上,即蛇绿岩是作为前泥盆系基底出露的.     

Progress in the study of tectophysicochemistry

Tectophysicochemistry is a research area that deals with the interrelations between physical and chemical changes of crustal materials caused by tectonism. A given tectonic force may be resolved into two parts: homogeneous stress and differential stress. Homogeneous stress refers to isotopic pressure, which is superimposed on the original pressure and affects the equilibrium of various chemical reactions. It is also a factor that influences petrogenesis,metallogenesis and metamorphism. Differential stress is commonly produced when external forces act on a given solid body. It may cause deformation of crustal materials and generate various kinds of structural features. Tectophysicochemistry pays special attention to pressure, temperature and other physicochemical conditions produced or induced by tectonism and studies the influences of additional tectonic parameters on various chemical equilibria, so it gradually develops into an independent area of science.