1) the buried history
埋藏史图
2) burial history
埋藏史
1.
A discussion on hydrocarbon accumulation dating determined by homogenization temperature and burial history of fluid inclusions——An example from the Fushan depression,Beibuwan basin;
由流体包裹体均一温度和埋藏史确定油气成藏时间的几个问题——以北部湾盆地福山凹陷为例
2.
A study on the geothermal and burial history of Subei basin and its enlightenments on petroleum exploration in South basin, the southern Yellow Sea;
苏北盆地热史、埋藏史研究及其对南黄海南部盆地油气勘探的启示
3.
The burial history and models for hydrocarbon generation and evolution in the marine strata in southern China;
中国南方海相层系埋藏史类型与生烃演化模式
3) tectonic-burial history
构造-埋藏史
1.
On detailed research of tectonic-burial history,combine d with the apatife fission tracks testing and fluid inclusion analyses,and using the EASY%R_o numerical simulation,the paper reveals the evolution process,the tectonic episodes and the strength of hydrocarbon-generation of Pal eozoic source rocks.
基于详细的构造-埋藏史研究 ,并结合磷灰石裂变径迹测试及矿物包裹体分析 ,运用 EASY% Ro 数值模拟技术 ,深入研究了孔古 3井的古生界烃源岩的生烃演化历史 ,阐明了孔古 3井古生界生烃作用发生的构造期次、生烃强度 ,揭示了孔古 3井处古生界烃源岩曾发生过两次重要的生烃作用过程 ,分别发生在海西 -印支期和喜山晚期 ,而主要生烃作用发生在喜山晚期 ,并提出了孔店构造带是有望实现黄骅坳陷深层古生界找油突破的有利地区。
2.
Palaeozoic source rocks discovered in Qigu-1 well has undergone a complicated tectonic-burial history since they were formed.
基于详细的构造-埋藏史研究,并结合矿物包裹体分析,运用EASY％R_o数值模拟技术,深入研究了歧古1井的古生界烃源岩的埋藏史、受热史和生烃史,阐明了歧古1井古生界生烃作用发生的构造期次、生烃强度,揭示了歧古1井古生界烃源岩曾发生过多次重要的生烃作用过程,其主要发生在海西—印支期和喜马拉雅晚期,得出了主要二次生烃作用发生在喜马拉雅晚期的重要结论,并提出了歧口凹陷是有望实现黄骅坳陷深层古生界找油突破的有利地域。
4) Bury history of source rock
源岩埋藏史
5) burial evolution history
埋藏演化史
6) depositional and burial history
沉积埋藏史
1.
Three models of hydrocarbon generation and evolution in different tectonic areas are established with depositional and burial history of three wells in different areas,which are maturative source rock an.
根据塔里木盆地北部草湖凹陷-库尔勒鼻凸库南1井和满1井的实测烃源岩镜煤反射率Ro数据,结合其他钻井资料,采用Ro梯度与沉积速率相互验证反演沉积埋藏史及生烃史的方法,确定主要烃源岩的“生烃”窗口,并对研究区的地层剥蚀厚度进行恢复。
2.
On the basis of microscopic research, the depositional and burial history, petrology characteristics, pore texture, diagenesis and pore evolutionary features of the Triassic to lower-Jurassic reservoirs in Hami depression are analyzed systematically.
在微观研究的基础上,对储集层沉积埋藏史、岩石学特征、孔隙结构、成岩作用以及孔隙演化特征等进行系统分析,认为哈密坳陷三叠系至下侏罗统碎屑岩储集层成分和结构成熟度低,成岩作用属早期深埋晚期抬升型,孔隙类型组合是以残余粒间孔-少量溶蚀粒间孔-大量微孔隙-成岩缝为主的组合,孔隙结构差,成岩阶段大部分已进入晚成岩B亚期。
3.
The depositional and burial history of the source rocks may be divided into three types: steadly deep burial, equilibrium burial and ephemeral shallow burial types.
松辽盆地石炭 二叠系是烃源岩,沉积埋藏史可划分出持续深埋型、平衡埋藏型和短暂浅埋型3种类型。
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