1) 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。
2) 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
3) Preferable source rock area of Qingyi member
青一段有利油源区
4) 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
5) bitumen/source rock
沥青/源岩
1.
Gas/source rock and bitumen/source rock comparisons have indicated that,light hydrocarbon C_(6+7) compositions in the Sinian,Cambrian and Ordovician productive formations are almost the same.
遵义后坝奥陶系红花园组生物碎屑灰岩中发现油苗和沥青,经过气/源岩、沥青/源岩对比,震旦、寒武及奥陶系产层轻烃C6+7结构组成基本一致,奥陶系含油苗灰岩轻烃星图与震旦系泥岩、寒武系沥青砂岩星图较为相似,显示红花园组油苗主要来源于震旦系和下古生界过成熟或高成熟海相烃源岩,油气经历了较长距离的运移,得以在奥陶系中保存下来。
6) 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。
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】：
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