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According to the principle of strontium isotope stratigraphy, we attempt to determine the age of the boundaries for Campanian/Santonian and Maastrichtian/Campanian by 87Sr/86Sr ratios for Gamba section in southern Tibet.

在与国际上同期海相地层锶同位素演化曲线对比的基础上,研究了晚白垩世海相碳酸盐锶同位素组成与主要地质事件的关系;在将本研究锶同位素数据融入到全球中新代海水锶同位素曲线的基础上,综合作出了中新生代海平面变化和锶同位素对照曲线,讨论了全球风化速率,造山事件,气候,海平面变化以及灾变性事件对中新生代海水锶同位素的控制作用;根据锶同位素地层学原理,本研究尝试将碳酸盐锶同位素组成用于海相地层定年上,利用已有的全球海水87Sr/86Sr值-年龄数据库和测试的藏南晚白垩海相碳酸盐的87Sr/86Sr值,确定了岗巴剖面Campanian/Santonian和Maastrichtian/Campanian阶界线,标定了广泛分布于白垩纪的厚壳蛤化石的年龄;本研究还将这些方法推广到了塔里木盆地井下奥陶纪地层的年龄标定,确定了中/上,中/下奥陶统界线,从锶同位素角度获得了古岩溶作用证据,显示锶同位素地层学在解决海相地层对比,年龄确定及在岩溶型油气储层研究中的潜在价值和良好应用前景。

But the genesis of the carbonite reservoir rocks, the differences in lithology, diagenesis, post diagenesis, structural fractures and dissolution have made it difficult for the general concepts and methods of the flow units to be suitably used in fracture-and-cavernous carbonate reservoirs.

主要储集空间以构造变形产生的构造裂缝与岩溶作用形成的孔、洞、缝为主,其中大型洞穴是最主要的储集空间,裂缝既是主要的储集空间,也是主要的连通通道。塔里木盆地塔河碳酸盐岩油田即属于此类油藏。

It deepens the previous view that the alteration of conodont faunas was controlled by water depth and water temperature.

这一观点深化了塔里木盆地奥陶纪牙形石动物群分区及类型演替的成因机理。

The collection for conodont samples of the Ordovician was carried out in the platform facies region of the Tarim Basin. Sixteen outcrop sections were sampled systematically and 29 well drillings were collected at the important intervals. More than 600 samples were acidized, and thousands specimens were obtained.

塔里木盆地台地相区奥陶系16条露头剖面进行了系统的牙形石样品采集,对29口钻井岩心的重点层段进行了牙形石样品采集,分析了采得的共600余块样品,在奥陶系各个层段都得到数量可观的牙形石。

Based on the conodont data, the evolutionary sequence of the Ordovician conodonts in the platform facies of the Tarim Basin was cleaned, one assemblage and 7 biozones are revised. After the cleaning, there are 1 assemblage and 20 biozones across the Ordovician in ascending order in the platform facies region of the Tarim Basin.

基于所获得的牙形石系统资料,对塔里木盆地奥陶纪台地相区已建牙形石生物地层序列进行了清理,确定了1个牙形石组合和20个牙形石带,据新的资料对8个原有的生物地层单元作了厘定。

The discovery of the Silurian- Devonian oil and gas reservoir reveals a good exploration prospect.

塔里木盆地志留-泥盆系油气藏的发现,展示了志留-泥盆系良好的勘探潜力。

The strata and lithological traps of Devonian and Silurian are the exploration targets in LS area, Tarim Basin.

塔里木盆地LS地区,泥盆系和志留系的地层圈闭和岩性圈闭是重要的勘探目标。

The southern part of Kuche County is located to the south of Tianshan Mountain, the edge of diluvial fan and the area of alluvial plain.

自然地理概况库车县南部地区位于天山南麓、塔里木盆地北部的渭干河洪积扇扇缘及冲洪积平原地区,北距天山约120km,南距塔里木河10余km。

The dust devil and fly ash which happened from Tarim Basin to the west of Hexi Corridor on May 13~14th in 1999 is analyzed with the data from FY-1C meteorological satellite launched recently in China.

利用我国新近发射的风云-1C极轨气象卫星,对1999年5月13~14日发生在塔里木盆地至河西走廊西部的沙尘暴与浮尘扬沙天气进行分析。

Therefore,it was analyzed that space-timedistribution rule,the relationship among the quantity of dustfall and meteorologicalelements,aeolian erosion.

由此研究塔里木盆地降尘的时空分布规律,降尘量与气象因子、风蚀的关系。

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