1) K1qn1 mudstone
青一段泥岩
1.
Difference of formation and evolution of overpressure of K1qn1 mudstone east and west of Daqing placanticline;
大庆长垣东西两侧青一段泥岩超压形成与演化的差异性
2) K1qn1 source rock
青一段源岩
1.
Based on the study of K1qn1 source rock development and hydrocarbon-expulsion characteristics,overpressure and its distributing characteristicss,T2 source fault and its distributing characte-ristics of Fu-Yang oil layer in Sanzhao depression,the match of source rock,overpressure and fault and its controlling effects on hydrocarbon accumulation and distribution have been studied.
在综合研究三肇凹陷青一段源岩发育及排烃特征、超压及分布特征和T2源断裂及分布特征源岩、超压和断裂空间匹配关系对油成藏与分布控制作用的基础上:认为青一段源岩和其内超压空间匹配控制着三肇凹陷扶杨油层油成藏分布范围,超压和T2源断裂配置控制着扶杨油层油聚集深度和层位,超压和T2源断裂平面配置控制着扶杨油层油聚集的部位。
3) K1n1 mudstone
嫩一段泥岩
1.
By use of the changes of acoustic logging data with buried depth and equivalent depth method,formation and evolution characteristics of overpressure of K1n1 mudstone in the north of Song-liao Basin was studied.
利用声波时差随埋深的变化及等效深度法,对松辽盆地北部嫩一段泥岩超压大小、分布特征及形成时期进行了研究。
4) dark mudstone in Es_1 Member
沙一段暗色泥岩
6) Qing I Member
青一段
1.
Study on oil and water zones distribution rules and interpretation method for Qing I Member in Yingtai-Bayanchagan area;
英台巴彦查干地区青一段油水层分布规律及解释方法研究
补充资料:巫山一段云 青郊送客
【诗文】:
野寺松花落,晴川柳絮飞。临风白马紫金袜,欲去惜芳菲。聚散今犹古,功名梦也非。青山不语暗相讥。谁见二疏归。
【注释】:
【出处】:
野寺松花落,晴川柳絮飞。临风白马紫金袜,欲去惜芳菲。聚散今犹古,功名梦也非。青山不语暗相讥。谁见二疏归。
【注释】:
【出处】:
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