华南基底变质岩的Sm-Nd同位素及其对花岗岩类物质来源的制约   总被引：33，自引：17，他引：33  

沈渭洲  朱金初  刘昌实  徐士进  凌洪飞 《岩石学报》1993,9(2):115-124

华南地区存在两种类型变质基底。Sm-Nd同位素数据的研究结果表明,它们可分别代表华南两种类型元古代地壳端员。华夏地块区副变质岩代表成熟度较高的(早)元古代地壳端员,~(147)Sm/~(144)Nd=0.1198,~(143)Nd/~(144)Nd=0.511822;江南古岛弧区副变质岩代表成熟度较低的(中—晚)元古代地壳端员,~(147)Sm/~(144)Nd=0.1246,~(143)Nd/~(144)Nd=0.512170。根据上述数据得出了华南元古代地壳Sm-Nd同位素演化域,进而对华南不同时代花岗岩类的物质来源作了进一步的讨论。  相似文献   

On some problems about testing stochastic models of the earthquake time series     

Gerassimos A. Papadopoulos 《Natural Hazards》1993,7(2):99-108

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中国油气区大地构造的历史因果论分析   总被引：2，自引：0，他引：2  

魏洲龄 《大地构造与成矿学》1993,17(1):1-12,38

依历史因果论大地构造学观点,就体现历史特点的大地构造体制来说,可将中国的油田划分为地槽型,地台型及地洼型三种类型,以现阶段的动力环境而论,则可将中国油气区划分为地幔汇聚型油气域和地幔扩散型油气域,并可进一步暂分为四大油气区,即陆缘海扩张型壳体油气大区,东部拉张型壳体油气大区,中部张一压型壳体油气大区和西部挤压型壳体油气大区,各大区成油气建造组合的大地构造类型,油气形成条件、油气藏类型、产出特点及分布规律等方面均有较大的差异。这些差异与各壳体的大地构造演化历史、壳体运动过程和动力学性质,以及各壳体的深部地质条件有密切关系。  相似文献   

重视和加强中国东部地区土地退化整治研究   总被引：2，自引：0，他引：2  

郑度  卢金发 《地球科学进展》1994,9(5):1-5

根据《２１世纪议程》土地荒漠化定义，从全球环境研究角度，论述了中国东部湿润、半湿润地区土地退化及其危害和开展中国东部地区土地退化研究的必要性和可行性，并提出了点面结合的初步研究设想。  相似文献   

金矿床定年方法进展及中国金矿床成矿时代   总被引：5，自引：0，他引：5  

王义文 《地质科技情报》1994,(2)

本文汇集和讨论了夹皮沟、辽宁、冀东、张家口、小秦岭、胶东、湘西、粤西－海南、滇西、北疆和台湾等我国主要金矿化集中区某些典型矿床的成矿年龄．在此基础上讨论了金矿床蚀变矿物、流体包裹体、石英、水热锆石、裂变径迹和矿石矿物同位素年龄测定新方法及热释发光技术在金矿床定年中的进展。普通铅模式年龄的定年意义是很有限的，但异常铅模式研究可用来示踪金矿化历史。＂成矿物质来源年龄老，矿床定位年龄新＂，即成矿作用具有明显继承性是中国金矿床最突出的特征。  相似文献   

中国早石炭世四射珊瑚动物地理分区   总被引：1，自引：0，他引：1       下载免费PDF全文

江茂生  何心一 《地质科学》1994,(3):228

 以中国主要地区早石炭世四射珊瑚化石资料为依据,采用传统的综合比较法与二态聚类分析方法相结合,把中国早石炭世四射珊瑚归为两大动物地理区,即特提斯大区和岗瓦纳大区,其中特提斯大区东部中国部分可再分为四个亚区:(1)华南亚区;(2)滇西亚区;(3)西南亚区;(5)北方亚区。  相似文献   

皖南晚元古代碰撞造山带构造轮廊   总被引：2，自引：0，他引：2  

马荣生  王爱国 《安徽地质》1994,(Z1)

本文从浅变质岩系与震旦系休宁组底砾岩之间的角度不整合以及这一构造面之下浅变质岩的大量同位素测龄成果资料和晚元古代花岗闪长岩、花岗岩带的形成等地质事实，论证了江南古陆晚元古代造山作用。提出皖南地区晚元古代造山运动经历了早期俯冲和晚期碰撞两个阶段，晚期碰撞造带可以划分为羊栈岭前陆褶冲带、障公山构造混杂岩带、白际岭岛弧仰冲带三个构造单元和若干个次级单元。  相似文献   

CHINA''S REGIONAL DEVELOPMENT IN THE 1980s     

Liu Xiaojin 《地理学报(英文版)》1994,(Z1)

l.Introducti0nIntheseveraldecadestilltheendofthe1970s,therewasnoanyleastd0ubtthatChinahadbeenfollOwingabalancedregi0naldevelopmentstrategy.0bligedtotlledolnesticandinternationalsituationofthattime,capitalinvestlnentxvasn1ost1yf0rcedt0beputintotheundevel0pedarea(westeconomiczone),thisstrategyprovedtobelesseffectiveandincurredahugelossofinvestmentbenefit.Althoughthewestzoneisabundantinnatllralresources(mineral,energyresourcesetc.),thelevelofregionaldevel0pmentfromeastzonet0westzoneisgradua1lydec…  相似文献   

International study onArtemia. L. Review of the literature onArtemia from salt lakes in the People's Republic of China     

George V. Triantaphyllidis  Bo Zhang  Lixiang Zhu  Patrick Sorgeloos 《International Journal of Salt Lake Research》1994,3(1):93-104

This literature survey covers data on the distribution, genetics and biology ofArtemia from the People's Republic of China (P. R. China) and the use of the brine shrimp in aquaculture and salt production. The vastness of the territory, the unfamiliar geography and the diversity of the habitats, have often lead to ambiguities and contradictions, leaving a gap in our knowledge about the Chinese populations ofArtemia. However, information aboutArtemia from P. R. China has recently become available and this is an attempt to summarize it.International interdisciplinary study onArtemia populations coordinated by the Laboratory of Aquaculture &Artemia Reference Center, University of Ghent, Belgium.  相似文献   

Early-Holocene geochemical evolution of saline Medicine Lake,South Dakota     

Katrina Allen Kennedy 《Journal of Paleolimnology》1994,10(2):69-84

Medicine Lake is a highly saline, meromictic, magnesium sulfate, closed-basin lake in northeastern South Dakota. The geochemical, mineralogical, and magnetic stratigraphies of sediments deposited from about 10.8 to 4.5 ka B.P. document the evolution of the saline brine in response to climatic change in the early to mid-Holocene. During the spruce occupation of the Medicine Lake catchment (10.8–10.0 ka B.P.), dark-grey massive basal sediments with low total-sulfur and carbonate content, upwardly increasing organic-carbon content, and high magnetic susceptibility were deposited in a deep freshwater lake. As the vegetation in the area changed from spruce to birch to oak and elm and finally to prairie between 10.0 and 9.2 ka B.P., and as the lake became shallow and salinity increased from <2 to >10%, light-and dark-grey calcareous and organic-carbon-rich banded sediments with low total-sulfur content and low magnetic susceptibility were deposited. Previous studies have shown that during the forest/prairie transition the lake then changed abruptly from fresh to saline as it lost a substantial portion of its volume. During the early prairie period (9.2–5.5 ka B.P.), alternating sections of aragonite-rich laminae and grey massive sediments with high total-sulfur content and multiple gypsum layers were deposited in a meromictic environment under conditions of fluctuating lake levels and salinity. Continued aridity during the mid-Holocene (5.5–4.5 ka B.P.) probably maintained the lake at relatively low levels and high salinity as dark-grey generally massive sediments with moderate total-sulfur, carbonate, and organic-carbon content and no measurable magnetic susceptibility were deposited.  相似文献