黄盛碧. 1994: 四川省小金—带奥陶纪大河边组的建立. 地质通报, (4).
    引用本文: 黄盛碧. 1994: 四川省小金—带奥陶纪大河边组的建立. 地质通报, (4).
    HUANG Sheng-bi. 1994: THE ESTABLISHMENT OF THE ORDOVICIAN DAHEBIANFORMATIONIN THE VICINITY OF XIAOJIN,SICHUAN PROVINCE. Geological Bulletin of China, (4).
    Citation: HUANG Sheng-bi. 1994: THE ESTABLISHMENT OF THE ORDOVICIAN DAHEBIANFORMATIONIN THE VICINITY OF XIAOJIN,SICHUAN PROVINCE. Geological Bulletin of China, (4).

    四川省小金—带奥陶纪大河边组的建立

    THE ESTABLISHMENT OF THE ORDOVICIAN DAHEBIANFORMATIONIN THE VICINITY OF XIAOJIN,SICHUAN PROVINCE

    • 摘要: 四川省小金县大河边、理县雪隆包、汶川下庄一带,出露一套浅海相碎屑岩及碳酸盐岩地层,该地层岩性特征明显,上、下层位关系清楚,具有可分性及可制图性,前人未建正式地层单位。笔者1992年在汶川下庄的结晶灰岩中采到了海百合茎化石,证实其时代属奥陶纪。因此,将该地层建立一个新的岩石地层单位─—大河边组。本文对大河边组的层型剖面进行了描述。

       

      Abstract: There outcrops a sequence of neritic clastic rocks and carbonate rocks at Dahebian,Xiaojin county,and Xia-zhuang of Wenchuan , Lixian county,Sichuan province.This sequence of strata shows distinct lithologic features andclear stratigraphic relationships with its overlying and underlying strata and is divisable and mappable. No formalstratigraphicunit has been set up for it. In 1992 ,the author found fossil crinoid stems in crystalline limestone at Xia-zhuang,Wenchuan,which were determined to be of Ordovician age. Therefore,a lithostratigraphic unit──the Da-hebian Formation──has been established for this sequence. This paper described the stratotype section of thisformation.

       

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