陕北奥陶系钾盐层位的发现与研究   总被引：6，自引：0，他引：6  

陈郁华  杜之岳 《地质论评》1998,44(1):100-105

陕北奥陶系是一个大型海相蒸发岩盆地,笔者在盆地东侧下奥陶统马家沟组,发现了钾石盐,光卤石等钾盐矿物,这是世界上首次在奥陶系发现钾盐,笔者较详细地研究了地质条件,含盐岩系剖面特下,物质成分和地球化学等,探讨了蒸发岩沉积的古地理环境和成盐模式据蒸发岩组成特征,结构构造,赋存状态,组合关系,地球化学诸方面的综合研究,认为陕北盆地钾盐沉积形成于残留卤水湖和干盐湖阶段。  相似文献   

Distribution and Significance of Carbazole Compounds in Palaeozoic Oils from the Tazhong Uplift, Tarim   总被引：3，自引：0，他引：3  

LIU Luofu University of Petroleum  Changping  Beijing Zhou Jian Fei Zhenbi 《《地质学报》英文版》1998,72(1):87-93

Carbazole compounds in crude oils from the Tazhong uplift of the Tarim basin have been fractionated and detected and successfully used to study petroleum migration and trace source rocks in the study area. Alkylcarbazoles have been found in large amounts in the oil samples analyzed and alkylbenzocarbazoles detected in a small concentration only in part of the samples, but alkyldibenzocarbazoles have not been found in oils. Based on the distribution of G1, G2 and G3 of C2-alkylcarbazoles, the ratio of C3-carbazoles to C2-carbazoles and the relative amounts of alkylcarbazoles and alkylbenzocarbazoles, one can know that the vertical oil migration in the Tazhong uplift is generally from below upward, i.e. from the Ordovician through the Silurian to the Carboniferous. Evidently, source rocks in the uplift should be lower Palaeozoic strata (Ordovician and Cambrian). This study shows that carbazoles are of great importance in the study of petroleum migration and source rocks.  相似文献   

The Crustal Structure and Assembly of Terranes in the Qaidam-Qilian-Beishan Area, Western China   总被引：2，自引：0，他引：2  

LIU Xun  GAO RuiInstitute of Geology  Chinese Academy of Geological Sciences  Baiwanzhuang Rd.  Beijing 《《地质学报》英文版》1998,72(3):243-255

Through a study of the geotransect from Golmud to Ejin Qi published recently, the tectonics of the crust beneath the area from the northern Qinghai-Tibet plateau (Qaidam and the Qilian Mountains) to the border between China and Mongolia and its structure, composition and tectonic evolution have been revealed, and abundant information about the deep structures has been provided. Based on the research into the geotransect, it is suggested that the crust in this area was formed by the assembly of the terranes in different geological stages. Following the formation of the Palaeo-Asian continent, the north part of the corridor of the transect became a part of the huge unifying continent by the end of the Early Permian. In the Mesozoic and Cenozoic, as a result of the compression mainly by the push of the Qinghai-Tibet plateau on the south, the unique crustal structure and geomorphologic features on the northern Qinghai-Tibet plateau were formed. This geotransect together with the Yadong-Golmud geotransect co  相似文献   

塔中地良奥陶系地层格架与沉积演化   总被引：1，自引：0，他引：1  

贾进华  顾家裕  李小地  周东延 《海相油气地质》1998,(4)

塔里木中部地区奥陶系大致以Ⅰ号断裂为界分东北和西南两个地层分区,自下而上分白云岩段、灰岩段、泥质灰岩段、泥岩夹灰岩段、泥岩夹砂岩段、砂砾岩段、泥岩夹砂岩段、泥岩灰岩互层段和砂岩段等9个岩性段。早奥陶世,塔中地区以碳酸盐岩台地相为主,自西向东为局限台地相、开阔台地相、台地边缘相和深水斜坡相。中——晚奥陶世,塔中地区西部以混积陆架相为主,东部以深水斜坡相为主。中—晚奥陶世,塔中东部及塔东地区在构造上具弧后前陆盆地性质。中—上奥陶统地层完整地记录了该盆地从形成发展到消亡的过程,即早期为深水斜坡相复理石活动沉积,晚期演化为浅海陆架相稳定沉积。  相似文献   

碳酸盐岩压溶埋藏史和排烃数值模拟模型初步探讨     

高岗  柳广弟 《海相油气地质》1998,3(2):55-58

压溶作用产生的缝合线是烃富集的场所及初次运移的通道。碳酸盐岩烃源岩压溶过程,随着地层厚度和体积的减小,未熟和低熟油气会伴随孔隙流体一同排出。根据碳酸盐岩埋藏与压溶机理,提出了压溶的碳酸盐岩缝合线或溶解缝厚度恢复及其古厚度恢复的数学模型,同时结合碳酸盐岩基质和缝合线孔度随深度的变化曲线建立了定量计算碳酸盐烃源岩压溶排烃量的数学模型。上述数学模型的关键是确定压溶作用开始和结束的深度和时间,缝合线的厚度  相似文献   

浙江桐庐冷坞二叠纪生物礁的发育模式   总被引：4，自引：0，他引：4  

吴亚生 《海相油气地质》1998,3(2):11-15

礁体底部具脉状层理的潮坪相碎屑沉积,礁体内部藻叠层岩夹层的存在,及礁体上部为煤系地层覆盖等都表明冷坞生物礁是一个典型的二叠纪岸礁;海绵骨架岩的存在表明它是个骨架型岸礁。  相似文献   

REANALYSIS OF PRINCIPAL COMPONENT ANALYSIS TO RESUME PAST VEGETATION AND ENVIRONMENT——Taking Fenzhuang Profile in Beijing as an Example   总被引：1，自引：0，他引：1  

张佳华 《中国地理科学(英文版)》1998,(3)

Ｉ．ＩＮＴＲＯＤＵＣＴＩＯＮＡｔｐｒｅｓｅｎｔ,ｇｌｏｂａｌｃｌｉｍａｔｅｃｈａｎｇｅｈａｖｅｂｅｅｎｗｉｄｅｌｙｐａｉｄａｔｅｎｔｉｏｎｔｏｉｎｔｅｒｎａｔｉｏｎａｌｙ．Ｃｌｉｍａｔｉｃａｎｄｅｎｖｉｒｏｎｍｅｎｔａｌｃｈａｎｇｅｓｆｒｏｍｌｏｃ...  相似文献   

Impacts of human activities on water cycles in Haihe Basin *     

LI Lijuan Institute of Geography  Chinese Academy of Sciences  Beijing CHINA 《地理学报(英文版)》1998,(3)

Ｉ．ＩｎｔｒｏｄｕｃｔｉｏｎｏｆＳｔｕｄｙＡｒｅａＨａｉｈｅｂａｓｉｎｃｏｖｅｒｓａｎａｒｅａｏｆ３１８０００ｋｍ２,ｃｏｎｓｉｓｔｉｎｇｏｆＨｅｂｅｉＰｒｏｖｉｎｃｅ,ＢｅｉｊｉｎｇａｎｄＴｉａｎｊｉｎ,ｍｕｎｉｃｉｐａｌｉｔｉｅｓａｎｄｐａｒｔｏ...  相似文献   

答《关于深海锰结核中“纳米级超微生物化石”的思考和建议》一文   总被引：2，自引：0，他引：2  

林承毅  边立曾 《高校地质学报》1997,3(2):236-240

本文详细讨论了东太平洋深海锰矿结核中新发现的中华微放线菌和太平洋螺球孢菌究竟是不是超微结构，首先，它们是笔者根据形态，结构和元素成分作为超微生物化石进行鉴定的，其次，透射电子显微镜中可以清楚地区分出完整的微生物结构，包括菌丝，孢子，孢囊和菌落等，它们之间的尺寸比例也是适当的，此外，透射电子显微像还揭示，深海锰质叠层石的纹层就是这些超微生物韵律性生长的结果，与滨海叠层中的纹层十分相似，笔者认为，已知微生物的最小尺寸不能作为否定新发现的超微生物化石的依据。本文还讨论了超微生物化石的术语问题。  相似文献   

山西大同煤田晚石炭世晚期和早二叠世早期植物群   总被引：3，自引：2，他引：3  

陈芬  王京东 《现代地质》1997,11(2):131-136,T002

对山西大同煤田晚石炭世晚期和早二叠世早期植物化石进行了研究，共鉴定植物化石２１属４８种，划分２个植物组合，讨论了植物群的特征和时代；此外，还论证了本区晚石炭世晚期和早二叠世早期植物群指示的古气候条件  相似文献