A MONGOLIAN AMBLYPOD IN THE RED BEBS OF ICHANG,(HUPEH)

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A MONGOLIAN AMBLYPOD IN THE RED BEBS OF ICHANG,(HUPEH)
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[1]杨鍾健.A MONGOLIAN AMBLYPOD IN THE RED BEBS OF ICHANG,(HUPEH)[J].Acta Geologica Sinica,1936,15(2):217-223.

[2]P. TEILHARD DE CHARDIN.ON THE OCCURENCE OF A MONGOLIAN EOCENE PERISSODACTYLE IN THE RED SANDSTONE OF SICHUAN, S. W. HONAN.[J].Acta Geologica Sinica,1930,9(4):331-332.

[3]C. Y. LIU.THE STRUCTURAL GEOLOGY OF SOUTHWESTERN HUPEH[J].Acta Geologica Sinica,1951(Z1):1-8,98,99.

[4]陈旭.THE DIVISIONS OF THE YANGSIN LlMESTONE IN SOUTHEASTERN HUPEH[J].Acta Geologica Sinica,1935,14(1).

[5]赵景波.THE STUDY ON THE RED SOIL OF NEOGENE IN XIAN AND BAODE OF SHANXI[J].Acta Sedimentologica Sinica,1989,7(3):113-120.

[6]Chen Qi,Chou Ganlin,Xue Linfu,Zou Xinmin,Zhou Heping,Du Yushen Changchun Geological College,Cbangchun,Jilin.PALAEOPLATE EVOLUTION IN THE SOUTHERN PART OF THE INNER MONGOLIAN OROGENIC BELT[J].Geological Review,1993,39(6):478-483.

[7]许杰.THE FAUNAS FROM ICHANG LIMESTONE[J].Geological Review,1948,13(Z2):265-265.

[8]LING Qiu,xian,), and ZHANG Xian,qiu,).PRELIMINARY STUDY OF THE RED BEDS IN THE HEYUAN BASIN OF GUANGDONG[J].Journal of Stratigraphy,2002,26(4):264-271,T003,T004.

[9]FU Sheng-yun,LI Ze-hong,ZHENG Zheng-fu.ORE-CONTROLLING CONDITIONS OF THE VEIN-TYPE LEAD-ZINC DEPOSITS IN THE CRETACEOUS RED BEDS IN FENGHUANG-MAYANG AREA IN THE SOUTHWEST EDGE OF YUANMA BASIN[J].Geology and Resources,2011,20(4):278-281.

[10]Ge Tongming,Liu Jian,Fan Limin,Zhang Shuixian,Wu Nengyou.MAGNETOSTRATIGRAPHY OF THE RED BEDS IN HENGYANG BASIN[J].Acta Geologica Sinica,1994,68(4):379-388.

[11]Wang Zhilong.THE RED BED-TYPE AND SANDSTOME-TYPE URANIUM DEPOSITS IN THE INLAND BASINS OF THE NORTHWEST CHINA[J].Uranium Geology,1988(4).

[12]Hao Qingzhen,GUO Zhengtang,Peng Shuzhen.A PRELIMINARY STUDY ON THE MAGNETIC PROPERTIES OF THE TERTIARY RED EARTH IN THE LONGXI AREA[J].Quaternary Sciences,2000,20(5):447-456.

[13]WANG Cheng-yuan.RESTUDY ON THE AGES OF SILURIAN RED BEDS IN SOUTH CHINA[J].Journal of Stratigraphy,2011(4):440-447.

[14]赵东旭.THE DISCOVERY OF PHOSPHATIC RED ALGAE IN THE SINIAN DOUSHANTUO FORMATION[J].Acta Sedimentologica Sinica,1986,4(1):126-127.

[15]胡瑞林　殷跃平.THE DISINTEGRATION FEATURES OF THE RED MUD IN THE THREE GORGES[J].Journal of Engineering Geology,2004,12(Z1):61-64.

[16]Wei Fucai.THE LOCATION OF THE RED CLAYEY SOIL IN GUILIN ON THE PLASTIC CHART[J].Carsologica Sinica,1988,7(2):153-159.

[17]李连捷.PHYSIOGRAPHICAL SIGNIFICANCE OF THE OCCURRENCE OF RED EARTHS IN NANNING BASIN KWANGSI[J].Acta Geologica Sinica,1936,15(4):529-554.

[18]LUO Jun-yan,LI Sheng-rong,YANG Su-ming,XU Yuan-liu,LI Cheng-lu,ZHANG Ju-quan,SONG Ji-ye.THE SIGNIFICANCE OF PARAMETERS OF FOURIER TRANSFORM INFRA RED DIFFUSED SPECTRUM IN MINERALIZATION[J].Journal of Mineralogy and Petrology,2009,29(1).

[19]CHENG Qiang,KOU Xiaobing,HUANG Shaobin,ZHOU Yongjiang.THE DISTRIBUTES AND GEOLOGIC ENVIRONMENT CHARACTERISTICS OF RED BEDS IN CHINA[J].Journal of Engineering Geology,2004,12(1):34-40.

[20]Qiao Yansong,Zhao Zhizhong,Li Zengyue,Wang Yan,Fu Jianli,Wang Shubing,Li Chaozhu,Yao Haitao,Jiang Fuchu.AEOLIAN ORIGIN OF THE RED EARTH FORMATION IN THE CHENGDU PLAIN[J].Quaternary Sciences,2007,27(2):286-294.

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.1936. A MONGOLIAN AMBLYPOD IN THE RED BEBS OF ICHANG,(HUPEH)[J]. Acta Geologica Sinica(),15(2):217-223

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