【两广地质调查所特刊】七 - 两广地质调查所编辑部.pdf
多故葛氏作古地理圖時即以中泥盆靶之欧亞大海相連絡喜馬拉亞大内斜HglaaGeosynelne為通道 矣况葛氏及其他古生物家與法雷西8學者之意見亦中國泥盆紀化石興西欧所產相似者殊 g及東京Ho處所發见之下泥盆化石相似果爾则中國泥盆之海浸當不自中泥盆始 西修仁探回之腕足類化石之結果確其為下泥盆紀物舆歐洲來因河流域Ralan亞洲之西比利 葛利普教授Qraga所著之中國史内已远及之但葛氏中國下泥盆之海相沈尚付缺如雲南束 十八年馮景蘭李殿臣二君修仁之調查其增盆吾人對于泥盆之知識当不少至若泥盆地層之劃分 現雨廣泥盆紀地層分怖甚廣廣西所產化石尤豐富而完美如民十七年樂森君象縣東网嶺之探集興民 Vop Loos
LIANG-KWANGTI-CHIIHTIAO-CHA-SO THECEOLOGICALSURVEYOFKWANGTUNGKWANGSI CHUCHHAHUADIRECTOR.SPECIALPUBLICATION NO.APRELIMINARYREPORTONTHE IDENTIFICATIONOFSOMELOWER DEVONIANBRACHIOPODSAND PELECYPODSOFKWANGSI PROVINCE(With2plates) HSICHIH CHANG CaNTON,CHiNa.
DirectoroftheGcologicalSurveyof ChinaatPepingandMr.Chu Ting-ooGeologistof theGeologicalSurvey of Kwangtung and Kwangsi have studiedthegeologyof Yunnan for manyyears.TheircollectionsoftheDevonianBrachiopodshavebeenstudied byProfessorA.W.GrabauandMr.ChaoYatsengrespectively.