1) the second Member of Baigang Formation
百岗组二段
1.
Based on data of the well logging,drilling core,thin section microstructure,seismic attributes,the authors analyse the petrology combination,sedimentary structure,section structure,biological fossil,logging facies and seismic facies of the second Member of Baigang Formation.
通过对研究区内100余口钻井测井资料的综合分析、20余口钻井岩心的详细描述、700多块薄片的详细鉴定,并充分利用地震资料,综合分析了研究区百岗组二段的岩石组合、沉积构造、剖面结构、生物化石、测井相和地震相等特征,认为研究区百岗组二段发育了扇三角洲和湖泊两种沉积相,扇三角洲主要发育在研究区的西北部和东北部,湖泊沉积相主要发育在研究区的南部。
2) Baigang formation
百岗组
1.
Sequence stratigraphy and sedimentary evolution of Nadu formation and Baigang formation of the Paleogene in Baise Basin;
百色盆地古近系那读组和百岗组层序地层划分与沉积演化
2.
The studies of the depositional characteristics showed that there are two different sedimentary systems in Baigang Formation in the eastern depression of Baise basin.
通过详细研究百岗组沉积相发育特征,将三角洲进行不同类型划分,认为百色盆地东部坳陷的南北两侧分别发育两套不同的沉积体系。
3) The 1st and 2nd member of Funing Formation
阜宁组一段、二段
4) The second member of Kongdian formation
孔店组二段
5) Member 2 of Shanxi Formation
山西组二段
1.
Sedimentary sequence and tectonic features of outcrops and cores in Member 2 of Shanxi Formation in the east edge of Ordos Basin are studied with modern sedimentary mechanisms.
从露头分析和岩心观察入手,应用现代沉积学原理,对鄂尔多斯盆地东缘山西组二段露头和盆内岩心中的沉积序列及构造特征进行详细描述。
补充资料：雁荡山百岗尖
位于灵岩景区北端，为雁荡山主峰，由三尖合成，东尖较低，西尖最高，海拔1150米。登临峰顶，可俯瞰全山风景。举目遥望，数县河山，万里东海，尽收眼底。“百岗云海”如波汹涛涌，变幻无常, 景色壮观，令人神往，常与“雁湖日出”并提。它与雁湖尖、凌云尖、乌岩尖，合称雁荡四大尖。百岗尖山高崖陡，过去游人少至。现有车路通达，欲登高一览，可从大远鼋坑沿盘山车路而上，或乘坐汽车直上山顶。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条