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1)  Fangniushan section
放牛山剖面
2)  Fangniushan
放牛山
1.
Fangniushan quartzite series consist of coarse terrigenous clastic rock which has been suffered the metamorphism of low green schist facies,contact lines of its top and base are distinct.
放牛山石英岩系为经低绿片岩相变质的粗陆源碎屑岩。
3)  Meishan section
煤山剖面
1.
From high resolution magnetostratigraphic study of the Meishan section of Changxing County, Zhejiang Province, the following conclusions are obtained: (1) The Meishan section can be divided into five normal polarity subzones and four reversed polarity subzones.
通过对浙江长兴煤山剖面的高分辨率磁性地层学研究,得出以下结论:(1)浙江长兴煤山剖面可划分为5个正向极性亚带和4个反向极性亚带。
2.
Based on detailed investigation of the sedimentology and conodont faunas on the Permian_Triassic boundary strata of the Meishan section, Zhejiang Province, South China, a new paleoecological model about two important genera Hindeodus and Clarkina (or Neogondolella ) is proposed.
通过对浙江长兴煤山剖面二叠-三叠系界线层沉积相分析及牙形石演化规律研究,提出了该时期Clarkina(Neogondolela),Hindeodus两类重要牙形石属的生态新模式。
3.
The Dongling section can complement reptenished some deficiency of the Meishan section from its three features:ty.
parvus距界线粘土层顶面仅高出13cm,化石保存完好以及界线粘土层至P/T界线附近均为单一的灰泥岩三特点弥补煤山剖面之不足。
4)  Kongshan section
孔山剖面
5)  mountain profiles
山地剖面
6)  Jianshan Section
尖山剖面
补充资料:放牛经
【放牛经】
 (经名)一卷,秦罗什译。为增一阿含经放牛品之别译。以放牛之十一法譬比丘之十一法。
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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