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机构地区:[1]Lanzhou Institute of Geology, Chinese Academy of Sciences, Lanzhou 730000, China
出 处:《Science China Chemistry》1995年第1期85-96,共12页中国科学(化学英文版)
基 金:Project supported by the National Natural Science Foundation of China.
摘 要:It is beheved that the Shujiaba Formation belongs to a series of thick turbidites. 20 ichnogenera have been found in the formation, of which 14 genera were found in the Devonian System of China for the first time The ichnogenera are mostly of typical deep-water ones and belong to the Nereites ichnofacies A detailed study of morphology and behaviour of the trace fossils indicates that the Shujiaba Formation was deposited in a bathyal-abyssal environment.It is beheved that the Shujiaba Formation belongs to a series of thick turbidites. 20 ichnogenera have been found in the formation, of which 14 genera were found in the Devonian System of China for the first time The ichnogenera are mostly of typical deep-water ones and belong to the Nereites ichnofacies A detailed study of morphology and behaviour of the trace fossils indicates that the Shujiaba Formation was deposited in a bathyal-abyssal environment.
关 键 词:Nereites ICHNOFACIES terrigenous clastic turbidite series bathyal-abyssal sedimentary environment. DEVONIAN Shujiaba Formation NORTHERN BELT of WESTERN Qinling Mountains.
分 类 号:Q911[天文地球—古生物学与地层学]
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