最新刊期

    3 4 1982
    • 含油气盆地研究的关键问题

      Vol. 3, Issue 4, Pages: 291(1982) DOI: 10.11743/ogg19820401
      摘要:板块学说问世以来,地质学的各个领域几乎都受到了或多或少的骚动。论者谓板块学说乃最近十年来地球料学的一大突破,并预言地球科学的下一个突破将是"古海洋的突破"。诚然,"岩石圈及其动力学计划"问世之后,板块学说登上了大油,其中心环节端在于"消失在山脉中的古海洋。  
        
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    • 陆相生油是怎样提出来的

      Vol. 3, Issue 4, Pages: 292(1982) DOI: 10.11743/ogg19820402
      摘要:我在1941年曾写过一篇小论文,首次对只有海相才能生油的论点提出挑战,而认为陆相(湖相)是同样可以生油的。回顾一下写这篇文章的经过,可能是不无意义的。这篇文章是在1940年寒假写的,那时我在堪萨斯大学念了一个学期,刚学完石油地质这门课。  
        
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    • 老少和衷共登攀

      Vol. 3, Issue 4, Pages: 293(1982) DOI: 10.11743/ogg19820403
      摘要:欣逢中国地质学会六十周年大庆,我曾借《石油实验地质》的篇幅,献上七律两首,以表一个老会员的微薄心意。但笔拙情长,未尽欲言。现在趁这次笔谈会的机会,再说几点感想与希望。第一,按我国的传统,六十年算是甲子一周,标志着承先启后的新开端。用黄理事长的术语说,也就是一个"旋回"吧。  
        
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    • 建议成立一个全国性的油气勘探指导机构

      Vol. 3, Issue 4, Pages: 294(1982) DOI: 10.11743/ogg19820404
      摘要:祖国石油巨变,我是历史见证人之一。解放前我国只有台湾西部、陕西延长、甘肃玉门、新疆乌苏、四川南部等十几个小油气田,目前已经找到数百个油气田,建立了许多个大的、比较大的石油基地,石油年产量已从建国初期的世界第二十九位跃居第六位。但是当前的产量距祖国需要还相差很远。  
        
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    • 油气普查勘探中的几个有关问题

      Vol. 3, Issue 4, Pages: 295-296(1982) DOI: 10.11743/ogg19820405
      摘要:二十世纪八十年代,祖国社会主义建设,正向"四化"进军。与之相适应的石油普查工作,则要向"四新"进军,即向新领域、新类型、新地区和新深度进军,以改变储采比失调局面,为祖国四化建设提供更多的油气资源;并在学术上,建立我们自己的石油地质理论。  
        
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    • 南海石油勘探的回顾

      Vol. 3, Issue 4, Pages: 297-298(1982) DOI: 10.11743/ogg19820406
      摘要:中国地质学会已成立六十周年,这是艰难曲折的六十年,是人才辈出的六十年,是取得辉煌成就的六十年。海洋石油地质勘探和其它矿产一样,解放前只是一个萌芽,直到解放后才得到蓬勃发展,取得了丰硕的成果。即以南海而论,三十年代马廷英开始对现代珊瑚进行了研究;抗日胜利后,穆恩之是第一个踏上西沙群岛和南沙群岛进行地质调查的中国地质学家。  
        
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    • 发展油气储层地质学有利于我国的石油工业

      Vol. 3, Issue 4, Pages: 299(1982) DOI: 10.11743/ogg19820407
      摘要:解放前,我国的石油工业基础非常薄弱,一九四九年全国只有十余个小油气田。解放后,通过石油地质勘探和开发工作,已充分证明我国具有丰富的油气资源。一九六五年我国达到石油全部自给,迄今已有数百个油气田投入开发。  
        
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    • 成就巨大 前途光明

      Vol. 3, Issue 4, Pages: 300(1982) DOI: 10.11743/ogg19820408
      摘要:中国古代有光辉灿烂的文化和精湛的工艺技术,早在一、二千年以前就知道石油天然气的利用,宋代钻井深度达到200米,清代已达到1000米。但鸦片战争以后沦为半封建、半殖民地社会,近代石油工业得不到应有的发展,解放前一直依赖洋油过日子。1949年解放时我国原油年产量仅12万吨。  
        
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    • 总结经验,再接再励,发现更多的油气田

      Vol. 3, Issue 4, Pages: 301-302(1982) DOI: 10.11743/ogg19820409
      摘要:石油和天然气是重要的能源,对于我国的社会主义建设具有十分重大的意义。作为一名石油地质工作者,有责任去努力发现油气。这是光荣而又艰巨的任务。首先,我们对于中国的油气前景应该是乐观的,充满信心的。  
        
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    • 回顾与展望

      Vol. 3, Issue 4, Pages: 302-303(1982) DOI: 10.11743/ogg19820410
      摘要:中国地质学会成立已经六十周年了。在纪念这个有意义的日子里,回顾一下解放以来我国石油工业和石油地质事业的发展历史,对于我们进一步找油将会是有益的。解放前,我国原油仅仅年产十几万吨。石油勘探工作量少得可怜,石油地质的理论也十分薄弱。  
        
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    • TECTONIC EVOLUTION OF ORDOS BASIN AND ITS OIL AND GAS POTENTIAL

      Vol. 3, Issue 4, Pages: 304-315(1982) DOI: 10.11743/ogg19820411
      摘要:Ordos basin,located in the connected part of the western active belt and easternstable region of China,has gone through many episcdes of tectonic movements. The platform and geosyncline regimes of Ordos in earlier Paleozoic period were incorporated as a whole by Caledonian orogenic movement, and then uplifted and unified with North Chian platform in later Paleozoic. During Mesozoic, it gradually developed into an extensive intracontinental depression but uplifted again in Cenozoic with Hetao, Yinchuan, Lupanshan and Fenwei subbasins formed atound.  
        
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    • THE DISCOVERY OF A PALEOPOOL IN MAJIANG AND ITS GEOLOGICAL SIGNIFICANCE

      Vol. 3, Issue 4, Pages: 316-326(1982) DOI: 10.11743/ogg19820412
      摘要:Recently,the black sandstone in the 2nd member of Wengxiang group(S1-2wn2)in Majiang,Duyun,Dangzhai and Kaili regions in eastern Gui-zhou was studied by detailed field survey and a lot of laboratory tests, and was discoverde no other than bituminous sandstone. The bitumen, with which the pore spaces between asnd grains are filled, is a variation of petroleum.  
        
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    • HYDROCHEMICAL INDICATORS AND ITS APPLICATION TO PETROLEUM EXPLORATION

      Vol. 3, Issue 4, Pages: 327-334(1982) DOI: 10.11743/ogg19820413
      摘要:287 water samples were selected from Fuyu reservoir in southern part of Song-liao basin.Their data were processed by means of discriminant analysis.For this part of the basin,8 formulas of discriminant function and isograms of synthetic discriminant value R are given. Benzene and organic acid were determined with 50 water samples respectively, and threshold for waters from reservoir and nonreservoir are confined.  
        
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    • Vol. 3, Issue 4, Pages: 335-342(1982) DOI: 10.11743/ogg19820414
      摘要:Songliao basin has undergone tectonic uplift at the end of Qinshankou during earlier Cretaceous.The changes in stratigraphic thickness,the erosion and weathering surfaces as well as absence of paleentolagical zones reveal that various types of contacts such as conformity, disnonfatmily and uncnnfoxmity, exist in the area between Qinshankou and Yaojia Foxmalions. The Putachua reservoir was formed under the influence of the extent of erosnon zones, which has resulted in the formation of impartant sedimentary fades, such as Proluvial fens and fan deltas etc. The development of great quantitirs of these facies sueely could enhance the availability of lithological traps and consequently shouid giver rise to more prospective areas for petroleum. The existence of odap zones in the west part of this basin favors the discovering of new reservoirs of unconformit type.  
        
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    • A PRELIMINARY STUDY ON CHINA'S EOGENE TRANSITIONAL FACIES

      Vol. 3, Issue 4, Pages: 343-350(1982) DOI: 10.11743/ogg19820415
      摘要:There is a great deal of transitional facies developed between continents and seas during Eogene in China.Due to tectonic and geographic controls,these facies distributed from marine to continent in order of seashore facies, transgressed lacustrine facies and inflowed lacustrine facies, showing a semivircular belt of NE trend in eastern China and NW trend in western China.  
        
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    • Vol. 3, Issue 4, Pages: 351-359(1982) DOI: 10.11743/ogg19820416
      摘要:The perylene of some samples from certain basins of China is examed by means of GC/MS/computer system.The perylene fractions,which contain mainly the compounds of molecular weight 252,and are devoid of those less than 252, were separated from the sample exiracts by means of column chromatograpny and thin layer chromatography. Mass spectrogram of the perylene isolated by glass capillary gas chromatography in our researchs are identical with the standard one.  
        
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    • Vol. 3, Issue 4, Pages: 360-368(1982) DOI: 10.11743/ogg19820417
      摘要:Middle Ordovician sediments locally occurred at the western and southern margins of Ordos platform and are represented by sand-shale facies and carbonates respectively.They are formed in Qilian-Qinling marine trough and Weibei carbonate platform is line with comprehensive analysts of simple-factor based diagrams, facies sequence and charaetus of paleobiota of individual atratigraphical column. Weibei carbonatc platform has correspondingly been subdivided into backbeach Iagoonal zone, shallow-water beach zone and forebeach seaward-sloping Zone.  
        
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    • TRACE FOSSILS OF GUANLING FORMATION AND ITS SEDIMENTARY ENVIRONMENT

      Vol. 3, Issue 4, Pages: 369-378(1982) DOI: 10.11743/ogg19820418
      摘要:Evidence from sedimentary structures,rock types,body fossil and trace fossil associations is used to two depositional environments(lagoonal and tidal-flat deposits)in lower and middle parts of the Guanling Formation of Middle Triassic, Guizhou Province.  
        
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    • THE SUBDIVISION OF QUATERNARY AND ITS LOWER BOUNDARY IN BEIJING PLAIN

      Vol. 3, Issue 4, Pages: 379-387(1982) DOI: 10.11743/ogg19820419
      摘要:In 1979,we suggested that pliocene-pleistocene boundary in Beijing plain,based on the results of seismological and geological research,may be placed between the Pliocene Shunyi Formation and the Pleistocene Xiadian Formation, deter about 2.43 m.y.B.P. Since then, we have studied more cores, measured their CaCO3 content and thermolumlnescene; Micratektltes from the Zhnili Formation,insecte fossils of Diptera from the Xiadan Formation of well No,l in Shunyi have also been discovered. These are sound evidurces for the subdivision of Quaternary and the determination of its lower boundary in this area.  
        
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    • ON PREDICTION AND DETECTION OF FORMATION PRESSURE

      Vol. 3, Issue 4, Pages: 388-394(1982) DOI: 10.11743/ogg19820420
      摘要:Basic principles and methods are briefly descussed for determining abnor-mal formation pressure and the depth at which it might accur in considerationof the peculiarity of prospecting.Herein seismic seismic prediction before drilling, dc-index detecting in the courae of drilling and well-logging evaluation after drilling etc. are induded. This paper emphasizes on the determining of averpressure strata on the basis of the relationship of sonic transmission time (Δt) versus depth in axgillaceous rocks, and the quick estimating the value of abnormal formation pressate by means of equivalent stress. Finally, an example of a well section cutting through sandstone and mudstone of Tertiary system is given.  
        
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    • GEOLOGICAL STRUCTURES OF MAOSHAN AND ITS OIL PROSPECTING

      Vol. 3, Issue 4, Pages: 395-400(1982) DOI: 10.11743/ogg19820421
      摘要:There were three explanations about the geological structures of Maoshan.First,accustomed saying,Maoshan including the most southern area of Anhui and Ji-angsu was the main range of the foldings formed in Indo-China movement; second, by geomechanics, Maoshan waa considered as a combination of several diffuent struetural systems, the north-south axis of Ningzhen Mt. reflexed are, and too, to be unrooted; third, recently, geologists working in plate-tectonic field emphasized the "listric fault" formed by stresses wmprrssed from cast to west in southun China, and thus Maashan was one of the nappes.  
        
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