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《WELL LOGGING TECHNOLOGY》 1995-05
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On the Features of Gamma Ray Response to Acidic Volcanics and Its Application

Feng Baohua.  
The features of Gamma Ray response to Acidic volcanics and their geologic cause have been analysed in detail. The geologic occurence, composition and microelements content of acidic volcanic clay are different from those of normal terrigenous sedimentary clay. Accordingly, abnormal response features on Gamma Ray log are quite apparent because of the high content of radioactive elements and potassium. Volcanic-elastic rock is a new kind of reservoir. Identification of source rock,reservoir rock and drape with Gamma Rag log and determination of their lateral distribution range are of great significance for the prospective evaluation of theoilfield.
【CateGory Index】: P631.819
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【Citations】
Chinese Journal Full-text Database 3 Hits
1 Feng Baohua and Dong Ruli;TRACE ELEMENT GEOCHEMISTRY OF VOLCANICSEDIMENTARY CLAYSTONE AND ITS SOURCE MAGMA TYPE AND CHEMICAL DIFFERENTIATION MECHANISM[J];中国区域地质;1993-04
2 Hao Jisheng;New Discoveries in Jr Curve[J];阜新矿业学院学报(自然科学版);1992-04
3 Feng Baohua(Institute of Mineral Deposits,Chinese Academy of Geological Sciences);THE MANIFESTATION OF CLAY ROCK OF ACIDIC VOLCANIC ORIGIN ON NATURAL GAMMA-RAY LOGGING CURVE AND ITS APPLICATION TO EVENT STRATIGRAPHY[J];物探与化探;1990-06
【Co-citations】
Chinese Journal Full-text Database 10 Hits
1 Lu Bin;Qiu Zhen;Zhou Jie;Dong Dazhong;Wang Hongyan;Xue Huaqing;Zhou Shangwen;Langfang Branch of PetroChina Research Institute of Petroleum Exploration & Development;PetroChina Research Institute of Petroleum Exploration & Development;;The characteristics and geological significance of the K-bentonite in Wufeng Formation and Longmaxi Formation in Sichuan Basin and its peripheral areas[J];地质科学;2017-01
2 XUE Kai-xi;LIU Shuai;LIU Xiao-dong;HU Yan-xiang;BIOND Tiwari;WEI Yong-qi;LIANG Hai-an;State Key Laboratory for Nuclear Resources and Environment,East China University of Technology;Civil & Environmental Engineering Department,California State University;;Review of the Physical,Mechanical and Engineering Properties of Clay Rocks[J];科学技术与工程;2016-16
3 Lecai Xing;Mingzhong Zhou;Liang Qi;Zhilong Huang;State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences;University of Chinese Academy of Sciences;School of Geographical and Environmental Sciences,Guizhou Normal University;;Discussion on the PGE anomalies and source materials of K-bentonite(Bed 5) in the Lower Cambrian Meishucun section, Yunnan[J];Chinese Journal of Geochemistry;2015-03
4 WAN Bin;GUAN ChengGuo;ZHOU ChuanMing;MENG FanWei;PANG Ke;TANG Qing;RAO Xin;State Key Laboratory of Palaeobiology and Stratigraphy,Nanjing Institute of Geology and Palaeontology,Chinese Academy of Sciences;University of Chinese Academy of Sciences;;Petrologic and geochemical characteristics of K-bentonites from the basal Ediacaran in Yangtze Platform,South China and their geological significance[J];岩石学报;2013-12
5 ZHOU Ming-zhong1,LUO Tai-yi2,HUANG Zhi-long2,LIU Shi-rong2(1.School of Geographical and Environmental Sciences,Guizhou Normal University,Guiyang 550001,China; 2.State Key Laboratory of Ore Deposit Geochemistry,Institute of Geochemistry,Chinese Academy of Sciences,Guiyang 550002,China);Early Cambrian Volcanic Records in Guizhou Province, China and Their Geological Significances[J];矿物学报;2011-03
6 WANG Shuili,LIANG Shaoxian (Institute of Geology and Environment,Xi'an University of Science and Technology,Xi'an 710054,China);REE geochemistry of clay in coal measures of Shanxi Formation in the north of North China[J];煤田地质与勘探;2010-06
7 SU WenBo1,LI HuaiKun2,HUFF W D3,ETTENSOHN F R4,ZHANG ShiHong1,ZHOU HongYing2 & WAN YuSheng5 1 School of Earth Sciences and Resources,China University of Geosciences(Beijing),Beijing 100083,China;2 Tianjin Institute of Geology and Mineral Resources,China Geological Survey,Tianjin 300170,China;3 Department of Geology,University of Cincinnati,Cincinnati,OH 45221-0013,USA;4 Department of Earth and Environment Sciences,University of Kentucky,Lexington,KY 40506-0053,USA;5 Beijing SHRIMP Center,Institute of Geology,Chinese Academy of Geological Sciences,Beijing 100037,China;SHRIMP U-Pb dating for a K-bentonite bed in the Tieling Formation,North China[J];Chinese Science Bulletin;2010-29
8 FENG Bao-hua( Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing, 100037 );SPECIAL FUNCTION OF THE NUCLEAR LOG AND THE APPLICATION OF ITS DATA TO THE REGIONAL GEOLOGIC SURVEY AND STRATIGRAPHIC STUDY——A NEW METHOD FOR THE STRATIGRAPHIC STUDY[J];地层学杂志;2005-S1
9 ZHANG Chao~1, MA Chang-qian~2, SHE Zhen-bing~1, YIN Kun-long~3(1.Graduate School, China University of Geosciences, Wuhan 430074, China;2.Faulty of Earth Sciences, China University of Geosciences, Wuhan 430074, China;3.Faulty of Engineering, China University of Geosciences, Wuhan 430074, China);Volcanic Ash in the Clay Rocks from Upper Shaximiao Formation of Middle Jurassic, Northeast of Sichuan Basin: Evidence from Petrology, Mineralogy and Geochemistry[J];高校地质学报;2005-03
10 WANG Shui-li,YAO Gai-huan (Xi′an University of Science & Technology Xi′an 710054,China);Geochemical characteristics of rare earth elements in I/S clay rocks in Late-Pateozoic coal measures of Northern China[J];煤田地质与勘探;2001-02
【Secondary Citations】
Chinese Journal Full-text Database 4 Hits
1 Feng Baohua (Institute of Mineral Deposits, Chinese Academy of Ceological Sciences);CARBONIFEROUS-PERMIAN TONSTEINS FORMED BY HYDROLYTIC REFORMATION OF VOLCANIC ASH SEDIMENTS IN NORTHERN CHINA[J];沉积学报;1989-01
2 Tan Tingdong(Academy of Oetroleum Exploration and Development ,Ministry of Petroleum Inlustry);THE RECOGNITION OF CLASIC SEOIMENTARY FACIES BYLOGGING TECHNIQUE[J];物探与化探;1988-05
3 Wei Kuishen;Tan Dehui;Electrofacies Study with Gamma Ray[J];测井技术;1988-05
4 Zhou Yiping (Kunming Institute of Coal Sciences)Burger Kurt (Rur Coal Company)Tang Dazhong (143th Party of Coal Geology and Exploration of Yunnan Province);A NEW DEVELOPMENT OF RESEARCH ON THE TONSTEINS(CLAY ROCK PARTINGS)IN LATE PERMIAN COAL MEASURES,SOUTHWEST CHINA[J];云南地质;1988-03
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