北极巴伦支海-喀拉海区地质构造特征及其石油地质意义

综合国际地质大会有关巴伦支海-喀拉海地区的最新研究成果,本文介绍了巴伦支海盆的地质、构造特征及其石油地质意义。巴伦支海-喀拉海区的地壳剖面自上而下分为沉积盖层、形变和褶皱复合体、结晶上地壳层-太古代-元古代花岗片麻岩和下地壳层;其沉积盖层可划分为下石炭系、上石炭系-下二叠系、三叠系、侏罗系、上白垩统-新生界5套沉积层,三叠纪、侏罗纪泥岩、二叠纪泥岩和白垩纪海相泥岩是主要烃源岩,储层有二叠纪、三叠纪和侏罗纪砂岩,尤其是三叠纪大型斜坡三角洲沉积体和中始新世砂岩是本区最重要储层。油气地质研究结果认为本区具有良好的油气潜力。     

青岛即墨温泉盆地热水沉积指示物及其标识性意义

经野外取样和XRD测试技术,在即墨温泉盆地发现硅质沉淀物、盐华、石膏、自然硫等温泉热水沉积指示物.根据热水沉积指示物的空间分布和含量的变化,阐述温泉热水沉积指示物的标识性意义：（1） 热水沉积指示物是划分第四纪沉积物层系的依据;（2） 是温泉地下热储温度的指示剂;（3） 依据热水沉积指示物百分含量的空间变化,可圈定温泉地热中心,指导地热资源开发;（4） 是寻找地下盲温泉和古地热水活动的标志;（5） 温泉热水沉积模式对现代海底热水沉积作用、成矿作用环境的模拟研究具有重要参考作用.     

春晖映万里 碧海铸利剑——中国海监东海维权执法支队成立两周年记

2008年5月13日,中国海监东海维权执法支队在上海挂牌成立,这标志着东海区海洋维权执法工作迈出了具有重要历史意义的一步。两年来,东海维权支队新一届领导班子坚持以邓小平理论、＂三个代表＂重要思想和科学发展观为指导,认真贯彻党的十七大精神,以＂团结协作、开拓创新、勤政廉洁＂为基本要求,团结和带领广大干部职工,     

继续巩固扩大学习实践成果

全省第一批深入学习实践科学发展观活动已经结束。半年来,省国土资源厅参加学习实践活动的各部门、各单位党组织,认真贯彻落实中央、省委和厅党组的要求部署,在驻厅检查指导组的精心指导下,扎实开展学习实践活动,取得了明显成效。这场具有重大现实意义和深远历史意义的活动,必将在我省国土资源管理史上留下浓墨重彩的一笔,谱写出我省国土资源管理工作科学发展的新篇章。     

The protoliths to the sillimanite gneisses from the Larsemann Hills and geological implication in their formation

The source rock from which the sillimanite gneisses derive mainly was the biotite plagioclase gneiss in the Larsemann Hills. It is the deformation-metamorphism process under special pressure and temperature condition, not the original rock compositions, that controls the presence of sillimanite. To a great degree, the sillimanite gneiss was the mixture of the detaining materials of the migrating felsic melt from the bt-plagioclase gneiss that underwent partial melting and the relics when the melt was removed. In sillimanitization the original rock had been changed substantially in chemical composition. The related metamorphism process severely deviated from the isochemical series, the process was of, therefore, an open system. In addition, the Al2O3 contents of the original rock was an important, but not critical factor for the formation of sillimanite, i.e., the sillimanite-bearing rock need not be of aluminum rich in composition, and vise contrarily, the aluminum rock may not produce sillimanite. The authors of the present paper postulate that the source rock from which the aluminum rich rock derives need not be of aluminum rich, but sillimanitization is generally the Al2O3 increasing process. The aluminum rich sediments such as clay or shale need not correspond directly to sillimanite-rich gneisses. No argillaceous rock present equals to sillimanite-rich gneiss in chemical composition. The protoliths to the sillimanite gneisses from the Larsemann Hills, east Antarctica, and their adjacent area may be pelite, shale greywacke, sub-greywacke, quartz sandstone and quartz-tourmalinite. If correct, the conclusion will be of significant implication for the determination of the sillimanite gneiss formation process and the reconstruction of the protolith setting.     

Heterogenous zircons from Mesozoic igneous rocks in the North China Craton and their tectonic implications

Based on a synthesis of zircon inheritance from Mesozoic igneous rocks in the eastern portion of the North China Craton （NCC） , it is proposed that inherited zircons with Neoproterozoie ages identified from these rocks are of a heterogenous derivation from the Yangtze/South China block, rather than from the NCC itself. The mechanism that introduces these zircons incorporated into the NCC is likely by tectonic underplating during the Triassic continental subduction of the Yangtze block beneath the NCC. Tectonic addition of abundant crustal materials represented by the heterogenous zircons into the NCC, probably along Moho or weak interfaces within the NCC＇s crust, led to the crustal thickening in the NCC. These heterogenous materials, either as （partial） source rocks or as contaminants of the magmas generated during an extension environment following the crustal thickening, were reworked and therefore have significant contribution to petrogenesis of the Mesozoic igneous rocks. The crustal thickening resulted from the tectonic underplating, as indicated by the distribution extent of the heterogenous zircons, is spatially similar to that of the lithospheric thinning, with both mainly occurring in the eastern segment of the NCC. This is probably suggestive of an intrinsic relation between the thickening and thinning events during the Mesozoic evolution of the NCC.     

推行土地登记代理制的意义

根据全国土地管理的形式要求,国家土地局在全国范围选定了几个大中型城市开展了土地登记代理制的试点工作。这项制度是根据我国目前的实际情况,借鉴国外成功经验而     

吉林省扶余县蔡家沟白垩系嫩江组断层脉状水的发现及其水文地质意义

受翼东水泥厂扶余公司的委托,对其水泥厂及周边进行水文地质条件评价,特别是对水泥厂范围内0.6 km2基岩裂隙水进行水质评价,水质符合饮用水标准,单井涌水量满足120 m3/d的要求。我们通过“多重环套法”的逻辑推理,从区域到局部再到点上的步骤分析与勘察,找到了优质断层脉状水,解决了生活用水的需要。1收集有关水文地质资料1.1地层和富水性第四系中更新统荒山组冲洪积层与冲湖积层,其富水性多在500 m3/d左右,但水质铁锰及氟化物超标,不适宜饮用。白垩系嫩江组孔隙裂隙水,富水性多在50 m3/d左右,但在断裂充水地段,富水性增强,单井涌水量100~30…     

永远忘不了的解放初期

1949年10月1日下午3时,在天安门城楼的开国大典上,毛泽东主席以他那浓重的湖南乡音向全世界庄严地宣告：“中华人民共和国中央人民政府,今天,成立了!”仅仅与他数尺之遥的我,作为香港《中国文摘》（CHINA DIGEST）半月刊的记者,正高举CONTAX相机,迅速捕捉每一个有历史意义的镜头,生怕漏掉一个珍贵的瞬间。     

镜铁矿矿物的找矿指示意义初探

对镜铁矿矿物的产出特征及其微量元素特征的初步研究,提出镜铁矿化是某些铁、铜、金、银、钨、锡、钼等矿化的重要找矿标志。