1) allodapic limestone
浊积灰岩
2) turbidity limestone
浊积灰岩
3) turbidity
浊积
4) turbidite
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
5) 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
6) 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
7) 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
8) 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.
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。
3.
Sha3 lower member in Langgu Sag is deep-water lacustrine deposit, and turbidite sand body reservoir of flood genesis is found in An421 well in Zhongchakou area.
廊固凹陷沙三下段为深水湖相沉积，局部发育洪水成因的浊积砂体。
9) turbidity channel
浊积水道
1.
Faces-controlling reservoir prediction of turbidity channel sandstone reservoir of Es_3 in Bonan subsag;
渤南洼陷沙三段浊积水道砂岩油藏相控储层预测
2.
A deep submarine canyon and turbidity channels were developed along the hanging wall of faulting break zone as a result of the 13.
8Ma前的强烈海退使得珠江口盆地白云凹陷发育了大型的海底峡谷—断裂坡折型深水扇,浊流沿海底峡谷将碎屑物向凹陷内搬运,在海底峡谷内充填形成浊积水道砂体,在断裂坡折带之下快速卸载形成前积砂体。
10) turbidite facies
浊积相
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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参考词条