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- ORDOVICIAN GRAPTOLITE BIOSTRATIGRAPHY OF GONGCHENG, GUANGXI, CHINA 广西恭城奥陶纪含笔石地层
- Graptolite biostratigraphy 笔石生物地层
- 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Unpublished Ph.D thesis of Peking University.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
- The black graptolite shale facies indicate a deep-water, half enclosed and anoxic sedimentary environment. 中奥陶世黑色的笔石页岩为典型的半封闭缺氧的深水沉积环境,反映了海水逐步加深,水体也变得相对宁静。
- These provide base for the correct measurement and valuing of graptolite reflectivity. 从而为笔石反射率的正确测定和取值奠定了基础。
- 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。
- The Ordovician graptolite bearing beds have been found from the core of Tadong 2 borehole in the northeastern Tarim Basin, Xinjiang. 塔里木盆地东部塔东2井岩心中新发现了一些奥陶系笔石化石,这些笔石标本呈炭质薄膜状,保存在该井4550。
- 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。
- 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]
- These 22 points are divided into two groups, which,represent respectiyely, two graptolite types in the early ordovician, namely, the South China type and the Central China type. 在平面图中,22个点可划分为2个点群,分别代表中国早奥陶世的两大笔石动物群,即华南型笔石动物群和华中型笔石动物群。
- 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。
- Focusing on understanding geological time, stratigraphy has made three milestone achievements characterized by lithostratigraphy, biostratigraphy and cyclostratigraphy. 摘要围绕对地质时间的认识,地层学取得了从岩石地层学、生物地层学和旋回地层学3次里程碑性的重大进展。
- Huang, T.-Y.(1977) Late Neogene planktonic foraminiferal biostratigraphy of the Tainan foothills region, Tainan, Taiwan. Petroleum Geology of Taiwan, 14, 121-145. 黄敦友(1977)台湾台南麓山带新第三纪浮游性有孔虫之生物地层。台湾石油地质,第14号,第121-145页。
- Yin Leiming and Yin Chongyu , 1997. Neoproterozoic Acritarch Biostratigraphy of China. In: Proceedings of The 30th International Geological Congress. Vol.11, pp. 67-73. 尹崇玉等,1997:华北地台南缘豫西鲁山洛峪口群洛峪口组宏观后生植物的新发现。地质论评,43卷(4):355
- SHA Jin-geng.Major achievements in studying the Early Cretaceous biostratigraphy of eastern Heilongjiang [J].Earth Science Frontiers, 2002,9 (3): 95-101. [9]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]
- NAN Run-shan, GUO Sheng-zhe, Paleozoic biostratigraphy and geography in the geosyncline of Inner Mongolia -Northeast [M].Beijing: Geological Publishing House,1992: 1-142. [4]南润善;郭胜哲.;内蒙古-东北地槽区古生代生物地层及古地理[M]
- We suggest that the strata are turbidite sequences that are deposisted on the passive continental margin.The strata containing plant, conodont and graptolite belongs to Early-Late Devonian. 该组中采获了低等蕨类植物、牙形石和笔石等化石,证实其时代属于早泥盆世-晚泥盆世。
- The Longmaxi formation of Lower Silurian is ten metres in thickness,containing three graptolite zones:Glyptograptus persculptus,Parakidograptus acuminatus and Orthograptus vosiculosus. 下志留统龙马溪组厚10m;含Glyptograptus persculptus;Parakidograptus acuminatus及Orthograptus vosiculosus三个笔石带.