1) turbidite mound
浊积丘
2) turbidite
[英]['tə:bi,dait] [美]['tɚrbɪ,daɪt]
浊积岩
1.
Formation mechanism of turbidite reservoirs in Sha3 member of Shahejie Formation,Dongying Depression;
东营凹陷沙三段浊积岩油藏形成机制
2.
Ordovician turbidite and its potential in gold exploration in Heilongjiang Province;
黑龙江省奥陶纪浊积岩及金矿床找矿远景
3.
Sedimentary characteristics of the turbidites and oil and gas accumulation in the secondary depressions in eastern China;
洼陷中浊积岩沉积特征及油气富集规律研究
3) turbidite fan
浊积扇
1.
The origin analysis of S3 segment turbidite fans in Westen sag,Liaohe depression;
辽河坳陷西部凹陷沙三段浊积扇体研究
2.
Relation between infilling patterns of short-term base-level cycle and macroscopic reservoir heterogeneity-taking Chang6 to Chang7 turbidite fan of Yanchang Formation in Longdong area as an example;
短期基准面旋回充填样式与储层宏观非均质性关系——以陇东地区三叠系延长组长6—长7浊积扇为例
3.
Analysis on genesis of turbidite fan of the Third Member of Shahejie Formation in the south of Huanxiling Oilfield;
欢喜岭油田南部沙三段浊积扇成因分析
4) turbidity sand
浊积砂体
1.
Quantitative study on key control factors for reservoir formation in turbidity sand;
浊积砂体油气成藏主控因素的定量研究
5) turbidite sandstone
浊积砂体
1.
The application of the log constrained inversion description technique for turbidite sandstones in Shinan area.;
测井约束反演技术在史南浊积砂体描述中的应用
6) turbidite sand body
浊积砂体
1.
A study on reservoir characteristics of the turbidite sand body Shasan intermediate member in Niuzhuang sag in Dongying depression;
牛庄洼陷沙三中亚段浊积砂体储集特征研究
2.
Application of the log constrained inversion in predicting the turbidite sand body in Niuzhuang area
测井约束反演在牛庄洼陷浊积砂体预测中的应用
3.
Statistic and regressive analyses have been carried out for petrophysical character and seismic attributes of known turbidite sand body in Es3 of Niuzhuang sub-sag.
对牛庄洼陷沙三段已知浊积砂体的岩石物性和地震属性进行统计、回归等分析,研究表明:①牛庄洼陷沙 三段不同岩性的速度具有一定差异,灰质砂岩速度最高,砂岩速度次之,泥岩速度最低;②反射振幅值太强和太 弱的浊积砂体,其储层物性都不好,根据其反射振幅值可定性地判断砂体储层物性;③全区难以确定统一的地 震属性与储层参数的对应关系,但同一个砂体,影响其反射振幅变化的外在因素基本相同,可应用回归经验公 式对其物性进行定量计算;④在利用地震属性预测储层物性时,不能片面、盲目地追求预测方法和计算模型的 普适性。
补充资料：浊积岩
| 浊积岩 turbidite 一种由浊流沉积作用形成的沉积岩。属半深海至深海沉积产物。按成分可分为：①钙质浊积岩。由碎屑灰岩和灰泥岩互层组成。②非钙质浊积岩。由砾岩、砂岩、粉砂岩和页岩互层组成。在纵剖面上，其特点是具鲍玛层序，即下部粗粒部分具粒序层理，其上具平行层理，再上具流水沙纹层理和包卷层理，顶部具水平纹层理，最上部为无层理的泥岩。底部常见各种印模，如槽模、沟模、锥模、重荷模等，也可见虫孔和叠瓦状构造。在碎屑石灰岩等粗粒部分含有底栖生物碎屑，在泥岩、灰泥岩等细粒部分见有浮游生物化石。一般不具有泥裂、雨痕、岩盐假象和原地植物根化石等浅水沉积物。大部分浊积岩都具有复理石建造和类复理石建造。 |
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