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- ORDOVICIAN CONODONT BIOSTRATIGRAPHY IN HEXIAN,ANHUI PROVINCE 安徽和县奥陶纪牙形石生物地层的研究
- MIDDLE AND LATE CARBONIFEROUS CONODONT BIOSTRATIGRAPHY OF NORTH CHINA 华北中、晚石炭世牙形石生物地层
- Keywords Taiyuan Formation;conodont Biostratigraphy;assemblage zone; 太原组;牙形石;生物地层;组合带;
- CONODONT BIOSTRATIGRAPHY NEAR THE LADINIAN-CARNIAN BOUNDARY INTERVAL IN GUANLING OF GUIZHOU 贵州三叠系拉丁阶-卡尼阶界线层牙形石生物地层
- DING Hui,WAN Shi-lu,LIANG Xiang-yuan.Preliminary study of Late Carboniferous conodonts biostratigraphy from Taiyuan Formation of Hebi,Henan[J].Shanxi Mining Institute Learned Journal,1983 (2):57-61. [8]丁惠;万世禄;梁湘元.;河南鹤壁晚石炭世太原组牙形石生物地层初步研究[J]
- CONODONT BIOSTRATIGRAPHY OF THE BAOERHANTU SECTION IN DARHAN MUMINGAN JOINT BANNER, INNER MONGOLIA 内蒙古达茂旗巴特敖包地区包尔汉图剖面牙形刺生物地层
- General Description of Conodont Biostratigraphy of Silurian System in Southwestern China 我国西南地区志留系牙形刺生物地层概述
- A Preliminary Study on the Ordovician Conodont Biostratigraphy at the Yakrik Section, Northwestern Margin of the Tarim Basin, Xinjiang 塔里木盆地亚科瑞克剖面奥陶系牙形石生物地层初步研究
- conodont biostratigraphy 牙形石生物地层带
- MEI Shi-long,1991.Middle and Late Cambrian conodont and trilobite biostratigraphy in Wanxian,Hebei.Unpublished Ph.D thesis of Peking University. 武桂春;2003.;鲁西地区晚寒武世牙形石
- According to the conodont and fusulinid fossils,their ages are determined to be Devonian-Permian. 根据所含化石确定地层形成时代为泥盆纪至二叠纪。
- Chi, W.-R.(1979) Calcareous nannoplankton biostratigraphy of the Nantou area, central Taiwan. Petroleum Geology of Taiwan, 16, 131-165. 纪文荣(1979)台湾中部南投区之超微体生物地层研究与对比。台湾石油地质，第16号，第131-165页。
- Huang, T.-Y.(1978) Foraminiferal biostratigraphy of the Hunghuatzu section, southern Taiwan. Petroleum Geology of Taiwan, 15, 35-48. 黄敦友(1978)台湾南部红花仔剖面之有孔虫生物地层学研究。台湾石油地质，第15号，第35-48页。
- Shaw, C.-L. and Huang, T.-C.(1996) Palynological biostratigraphy of the cretaceous sediments in Taiwan. Petroleum Geology of Taiwan, 30, 31-50. 萧承龙、黄增泉(1996)台湾白垩纪之孢粉生物地层。台湾石油地质，第30号，第31-50页。
- The Silurian strata containing abundant conodont fossils are well developed and comformable with the overlying Devonian strata in the Baizitian region, northern Yanbian, Sichuan. 四川省盐边县北部稗子田地区的志留系发育良好，牙形刺化石极为丰富，与上覆泥盆系连续沉积，并呈整合接触。
- SHA Jin-geng.Major achievements in studying the Early Cretaceous biostratigraphy of eastern Heilongjiang[J].Earth Science Frontiers,2002,9 (3):95-101. [3]沙金庚.;黑龙江东部早白垩世生物地层学研究的主要进展[J]
- Research on color index of conodont fossil shows that hydrocarbon source rocks in palaeozoic formation in Bachu Uplift Area are in mature phase of thermal evolution. 牙形刺化石颜色指标研究表明，巴楚断隆区古生代地层中的烃源岩正处在热演化的成熟期，寻找古生代油气藏应成为该构造带今后勘探的重点；
- The content of this text is studying evolutive degree of the source rock of the upper Sinian and the Paleozoic group mainly by vitrinite,pyrogenation,conodont and sporopollen. 以镜质体反射率、热解、牙形刺、孢粉作为划分的主要依据,研究了金衢盆地上震旦统和古生界烃源岩的演化程度。
- Micropaleontological experts An and Lee from China and Korea respectively,made an important contributions to the study of conodonts and biostratigraphy for their countries. 微体古生物学家安太庠和李河荣分别为中国和韩国的牙形学及其生物地层学研究做出了重要贡献。
- Chang, Stanley and Chi, W.-R. (1983) Neogene nannoplankton biostratigraphy in Taiwan and the tectonic implications. Petroleum Geology of Taiwan, 19, 93-147. 张锡龄、纪文荣(1983)台湾新第三纪超微化石生物地层与地质构造之意义。台湾石油地质，第19号，第93-147页。
