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1)  Dongganchi profile
东甘池剖面
1.
In the meantime,to understand the characteristics of LOI range of six zones in Dongganchi profile,the indications of LOI range to abrupt climate event and sediment landfor.
通过对北京地区房山东甘池剖面所取的197个样品的烧失量测定,结合14C测年、剖面岩性特征及孢粉序列分析,初步回答了烧失量作为沉积物有机质含量的代用指标,其数值波动对北京地区15000a以来环境变迁和气候变化的特征响应,同时针对房山东甘池剖面的6个带的烧失量变化特征,提出其在反映气候异常、沉积物地貌单元等的意义,从而为更好地重建过去气候和环境提供依据。
2)  Garzê-A section
甘孜-A剖面
3)  E-W section
东西剖面
4)  Dongpan section
东攀剖面
1.
Multidisciplinary stratigraphic data were analyzed from a well-preserved deep-water PTB section(Dongpan section) and used to define and correlate the PTB in Liuqiao area,Guangxi.
结果表明,东攀剖面上二叠系—三叠系界线处与煤山剖面具有较好的可比性:①东攀剖面放射虫A。
2.
The organic carbon isotope compositions were examined for the first time from a well-preserved deep-water PTB section(Dongpan section) in Liuqiao area,Guangxi.
研究了广西柳桥地区东攀剖面有机碳同位素的组成,并和浙江煤山剖面进行了对比。
5)  Donghu section
东湖剖面
1.
This article discusses the rock and biohorizon of the upper Jurassic according to the data of Donghu section in the north of Qiangtang Basin.
以测制的羌塘盆地北部东湖剖面为依据 ,对上侏罗统进行了详细的岩石及生物地层研究 ,将其划分为两部分 ,下部灰岩层为索瓦组 ,含Radulopectenfi brosus-Gervillellaaviculoides组合 ,时限为牛津期 ;上部灰岩、碎屑岩互层为白龙冰河组 ,含Radulopectenscarburgensis,Euprionoc erassp 。
6)  Dongling section
东岭剖面
1.
40 m)at the upper sector of the Changxing formation,in Dongling section of Northwest Jiangxi,and the Genus and Species charcteristics and abundances of the conodonds Clarkina changxingensis Clarkina deflecta assemblage zone at the lower stratum(The second bed,thickness 2 m;the noughth bed,thickness 8.
依据赣西北东岭剖面上二叠统长兴组上段第5层(厚34。
2.
The Dongling section can complement reptenished some deficiency of the Meishan section from its three features:ty.
东岭剖面可以它典型的H。
补充资料:开元寺东池早春
【诗文】:
池水暖温暾,水清波潋滟。
簇簇青泥中,新蒲叶如剑。
梅房小白裹,柳彩轻黄染。
顺气草薰薰,适情鸥泛泛。
旧游成梦寐,往事随阳焱。
芳物感幽怀,一动平生念。





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