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211.
Wang Hongzhen Zhai Yusheng You Zhendong China University of Geosciences Beijing China Shi Baoheng China National Petroleum Corporation Beijing China Yang Weiran Yang Guangrong China University of Geosciences Beijing 《中国地质大学学报(英文版)》2000,11(3)
On the occurrence of the celebration of the Fiftieth An-niversary for the establishm ent of the People’s Republic ofChina,we contribute this paper entitled“Developm ent of Ge-ological Science in China in the Twentieth Century”.Thiscomes out from a review of the newly published book aboutthe history of geological disciplines:“Fifty Years of Geologi-cal Science in China”.The draftof the paper was formed aftera discussion between the authors.It deals with the existingstate of geologica… 相似文献
212.
Peng Yuanqiao Tong Jinnan Faculty of Earth Sciences China University of Geosciences Wuhan China Shi Guangrong School of Ecology Environment Deakin University Rusden Campus Clayton Victoria Australia 《中国地质大学学报(英文版)》2000,11(3)
INTRODUCTIONThe L ower Yangtze sedimentary basin in South Chinawas a typical carbonate ram p slightly inclining northwestwardduring the Early Triassic. The rhythmic L ower TriassicGriesbachian is m ainly composed of thin- bedded mudrock andmarl (or lim estone) alternations,which can be observed overthe region.Due to the wide distribution and well- comparativestructures of these cyclic sedim ents,it was proposed that thesedim ents originated from som e periodic regional environmen-tal e… 相似文献
213.
CHARACTERISTICS OF VOLCANIC ROCKS AND ITS TECTONIC SETTING IN WESTERN PART OF LAZHULONG-JINSAJIANG STRUCTURAL BELT 相似文献
214.
GEOCHEMISTRY OF VOLCANIC ROCKS IN WESTERN PART OF JINSHAJIANG STRUCTURAL BELT AND ITS TECTONIC SETTING 相似文献
215.
DEPOSITIONAL SEQUENCES AROUND J/K BOUNDARY IN THE QOMOLONGMA AREA, SOUTH TIBET1 ShiX ,YinJ ,JiaC ,MesozoicandCenozoicsequencestratigraphyandsea levelchangesintheNorthernHimalayas,SouthTibet,China[J].NewslStratigr ,1996 ,33(1) :15~ 6 1.
2 LiuG ,WangS ,AdvancesintheUpperJurassictoLowerCretaceousstudyoftheTebetanHimalayas.PapStratigrPale ontol[M ].Beijing :GeologicalPress ,1987,17:143~ 16 6 .theNationalNaturalScienceFoundationofChina (No ..4982 5 … 相似文献
216.
THE NUMERICAL SIMULATE OF THE UPLIFT PROCESS OF THE QINGHAI—TIBET PLATEAU 相似文献
217.
THREE-DIMENSIONAL DEFORMATION ALONG THE ALTYN TAGH FAULT ZONE AND UPLIFT OF THE ALTYN MOUNTAIN, NORTHERN TIBET 相似文献
218.
Zhang Guomin Li Li and Shi YaolinCenter for Analysis Prediction CSB Beijing China Graduate School of Chinese Academy of Sciences Beijing China 《中国地震研究》1999,(4)
The relationship between the strain cumulative rate (i.e., the crustal strain rate, or CSR in short) and seismic activity is analyzed to develop a new method to determine risky regions for strong shocks within recent years by the recorded crustal strain field. Seismic activity, especially the recurrence period, is different in different areas. Ding Guoyu (1984) pointed out that, for different seismic regions, the difference in the recurrence period of strong earthquakes is mainly controlled by their difference in the rate of the tectonic movement, which is controlled by the seismogenic environment and the tectonic conditions. The method of determining the risky regions for strong shocks from the gradient of vertical strain rates observed in a geodetic survey is preliminarily tested with the earthquakes in recent years; the results show that this method is effective and useful for earthquake prediction. The relationship between CSR and seismicity in a specific region is studied with strain theories, obse 相似文献
219.
Intermsoftheresearchingermplasmandgeneticsofmarineanimals,Chinaseemsquiteweakincomparisonwithotherdevelopedcountries,fortherelevantresearchprogramswereonlyinitiatedinthe1980's.Inrecentyears,moreattentionhasbeendrawntothegermplasmsourcesofmarinevaluableanimalsandsomeresearchprogramshavebeenplannedorundertakeninChina.Abroad,thetechniquessuchaselectrophoresispatternsofisoenzym,RAPDandRFLPhavebeenappliedtotherelevantstudiesongeneticvariationandevolutionaryrelationshipswithinagroupofPenaeidshri… 相似文献
220.
It has been a period of time since the concept of scenario earthquake was proposed, but this concept has rarely been used in seismic safety evaluation in China since then. Meanwhile, because of the uncertainties of magnitudes-distances pairs, there is large arbitrariness while determining the envelope function of time histories in seismic hazard analysis. In this paper, we describe a method to control the envelope functions of the time histories by introducing the most-likely combinations of magnitude and distance of the scenario earthquakes based on a probabilistic method, revise the software of the ellipse model for seismic hazard analysis, and give a computation example. 相似文献