Isotopic Geochronology of the Xianghongdian Alkaline Complex, Northern Margin of the Dabie Mountains, China

To the north of the Qinling-Dabie orogen there exists a Mesozoic (K1) granite-syenite belt called the Beihuaiyang granite-syenite belt, in which the Xianghongdian alkaline complex outcrops in the Devonian Foziling schist and also intruded into the slightly earlier volcanic rocks. This alkaline complex is composed of syenite, alkaline syenite and nepheline syenite, but the nepheline syenite occurs inside the alkaline syenite in the pod-like, irregular, lenticular or layered shape. Researches on the petrogenesis of the alkaline complex and the relationship between the alkaline syenite and the nepheline syenite must rely on precise isotopic ages. Previous researches have reported iso-topic dating results merely by the 40Ar/39Ar method on hornblende and biotite separated from the alkaline syenite and nepheline syenite. In view of this, the authors have made fairly detailed isotopic geochronological studies of the alkaline syenite and nepheline syenite by using Rb-Sr isochron for the whole rock and minerals,     

Characteristics of Coal Accumulation of Transform-Extensional Basins in Linear Fracture Zones: A Case Study of the Meihekou Basin

This paper discusses the characteristics of coal accumulation of transfor-extensional basins in linearfracture zones on the basis of an analysis of tectonic evolution and sequence stratigraphy in the Meihekou basin.Coal accumulation of the basin occurred mainly in the accelerated rifting period of the transtentional regime and inthe late period of tectonic transformation of the transpressional regime. In the former period, swamps developed inshallow lakes. The thickness of coal seams was controlled by the activity of fault block. Thick coal was formed in adownfaulted trough. In the latter period, swamps developed in a braided fan delta plain. The coal seams are thin andhave poor lateral continuity. The thickness of coal seams was controlled by the migration of water channels in thebraided plain.     

海泡石活性土对食用菜油的脱色作用

海泡石粘以活化后,对食用菜油精制脱色效果良好,其活化工艺条件为：活化酸量８％,烘干温度１５０℃,活化温度１００℃,活化时间〉５ｈ液固比３：１。     

深层搅拌法在湘北地区的应用前景

本文扼要介绍了深层搅拌法的工艺技术及适用范围,对湘北地区的工程环境条件进行了分析讨论,认为在湘北地区推广这一施工技术不仅具备工程地质条件,而且有关十分广阔的应用前景。     

进行矿山开采经济效益分析充分利用矿产资源

针对当前有些矿山企业在经济不景气,导致采富弃贫,采易避难等不良现象,本文提出加强对采矿方法,选冶工艺流程,以及尾矿利用的综合分析研究,通过对矿产资源的充分利用来提高其经济效益,促进矿业经济的可持续发展。     

高喷灌浆技术在防渗加固长善垸浏阳河防洪大堤堤基中的应用

高喷灌浆在长善垸浏阳河防洪大堤第四系松散地基的防渗、加固中效果显著,与其它防渗措施比较,其施工速度快,成本低,在深度覆盖层堤基防渗中显示出无可比拟的优越性。     

郴州金船塘锡铋矿选厂工业流程的调整建议

本文通过对金船塘锡铋矿１００ｔ／ｄ选厂的流程考察,找出了存在的主要问题,提出了改进工业流程的有益建议。     

岳阳铁山灌区打山坡等引水隧洞工程地质问题及对策

岳阳铁山灌区的打山坡等３条引水隧洞,工程地质条件极为复杂,４１４队采用“新奥法”掘进,成功地解决了施工过程中遇到的严重片邦、冒顶和塌方等技术难题。     

我国水资源开发利用业绩与前景

新中国成立以来,我国水利事业得到迅速发展,有效地促进了社会的进步与经济的繁荣。我国是世界上人均水资源贫乏的国家之一,如何实现水资源与社会,经济、环境的协调发展,实现水资源的可持续开发利用,仍将是我国可持续发展的关键问题之一。回顾了新中国成立以来水资源开发利用发展的阶段与过程,简要介绍了在水资源开发利用与保护方面的主要成就,较为系统地回顾和总结了我国水资源管理方面的主要工作,并对２１世纪我国水资源可     

浅层地下水氯代烃污染天然生物降解的判别依据

天然条件下氯代烃生物降解的判别, 是确定氯代烃污染天然衰减恢复治理技术是否可以采用的关键, 可为天然衰减恢复治理技术的应用提供技术支持.通过分析氯代烃生物降解的特性发现, 地下水环境中氯代烃的生物降解, 必然伴随有第一基质、电子受体、中间产物以及有关的一些间接性指标, 在污染羽状体不同位置及污染羽状体内外产生明显变化, 这些指标的变化均可以不同程度地指示氯代烃生物降解的产生.据此总结出氯代烃生物降解衰减的判别依据分别为电子受体、第一基质(能源和碳源) 及降解中间产物三类指标.