FACILITATING REGIONAL SUSTAINABLE DEVELOPMENT THROUGH INTEGRATED MULTI-OBJECTIVE UTILIZATION, MANAGEMENT OF WATER RESOURCES IN THE LANCANG-MEKONG RIVER BASIN     

He Daming Centre for Environmental Evolution  Sustainable Development  Yunnan Institute of Geography  Kunming  China Hsiang te Kung Memphis University  TN  USA 《地理学报(英文版)》1997,(4)

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The Granite Pegmatites of Suchou   总被引：1，自引：0，他引：1  

Y. S.HUANG  Eormerly National Central University 《地质学报》1949,(Z1):157-170,184

I. INTRODUCTIONThe pegmatites discussed in this paper occur entirely in the granite region of Suchou (Wuhsien), Kiangsu and most of them are found within the marginal zone of the said igneous body. Although much work has been done on the Suchou granite by former geologists [19; 13; 21; 12], there is no literature dealing particularly with the pegmatites which are in intimate  相似文献   

A SUGGESTION OF A NEW METHOD FOR GEOLOGICAL SURVEY OF IGNEOUS INTRUSIONS     

李四光  仲揆 《地质学报》1924,3(2)

It may be safely presumed that few of us who have worked in the field as a geological surveyor would dissent in making an open confession of our unfortunate attitude towards igneous rocks particularly those of a massive form. These obstacles, as one is apt to regard them, are the unruly bodies  相似文献   

A GRAPHIC METHOD TO AID SPECIFIC DETERMINATION OF FUSULINOIDS AND SOME RESULTS OF ITS APPLICATION TO THE FUSULIN?E FROM N. CHINA.——WITH 2 PLATES AND 20 TEXT-FIGURES.     

李四光  仲揆 《地质学报》1923,2(Z2):51-94

本篇分为三节:第一节论研究(竹廷)蜗之方法及其各部分之名称;并猎取古生物学家迄今历史之结果而加以批评。第二节专述中国北部已发见之(竹廷)蜗。第三节讨论本篇所述各种(竹廷)蜗生存之时代及其棲息流徙之情形。  相似文献   

NOTE ON THE GEOLOGY OF CHANGSINTIEN-TUOLI AREA,S.W.OF PEIPING     

謝家榮 《地质学报》1933,(1)

Changsintien is a station on the Peiping-Hankow railway and is situatedabout 20 km S.W.of Peiping.Further S.W.for about 15 km is the townof Tuoli where begins the Tuotsin aerial ropeway for transporting coal and at  相似文献   

NOTE ON THE GEOMORPHOLOGY OF THE NORTH SHENSI BASIN     

謝家榮 《地质学报》1933,(0)

The geology of the north Shensi basin has been studied to some detail bythe American geologists Fuller,Clapp and others~1 in an oil exploration partysent out in 1914 under the joint auspices of the Chinese National Oil Administra-  相似文献   

OBER DIE PALAEOZOISCHE FLORA DER PROVINZ SUIYUAN~1     

斯行健 《地质学报》1934,(1)

Die palaeozoischen Pflanzen der Provinz Suiyuan sind bisher sehr wenig bekannt. Die in der vorliegenden Arbeit beschriebenen Pflanzen stammen aus dem sogenannten "Tachingshan Range" namentlich aus den Localitaten Tungshengmao und Kumenyintien. Die Fundorte liegen also etwa an der Grenze  相似文献   

ON THE OCCURRENCE OF AN INTERESTING FOSSIL WOOD FROM URUMCHI(TIHUA)IN SINKIANG~1     

H. C. SZE 《地质学报》1934,(1)

The fragment of fossil wood forming the main subject of this paper was collected by P. Teilhard de Chardin when he was sent to Sinkiang by the Geological Survey of China, with the Haardt-Citroen Expedition (1932).  相似文献   

栖霞石灰岩之腕足类化石     

赵亚曾 《地质学报》1927,6(2):83-83

本篇之结论有下列数要点.(一)德人佛莱士谓棲霞石灰岩属下石炭纪之说完至错误,其时代决非下石炭纪二)棲霞石灰岩在长江流域分布甚广,凡燧石石灰岩之底部无处无之,但自此南北行均渐归绝迹.(三)棲霞石灰岩代表-古太平洋区之海浸,故其生物化石海与南美洲者较相近而与我国北流及其他各处者反无关.(四)据腕足类化石之研究,棲霞石灰岩之时代应属上石炭纪,但为时在Schwagerina 期之前.(五)在长江流域,燧石石灰岩(即巫山石灰岩下部)代表-连续之沈积;底为珊瑚层(即棲霞石灰岩),属上石炭纪;中为各纺锤虫层,大致相当于Schwagerina期,属下二叠纪;上为Oldhamina及Lyttonia层,完圣与印度?领之上及中长身贝石灰岩相当,属中二叠纪。  相似文献   

An Unusual Porphyritic Texture of the Fangshan Granodiorite     

T.L.HO 《地质学报》1937,(Z1)

A remarkable character of the Fangshan (房山) granodiorite isthe abundance of the large phenocrystic orthoclase perthite throughoutthe central part of the igenous body. They project on the weathered  相似文献