1) west Lishui sag
丽水西次凹
1.
The Paleocene Mingyuefeng Formation, an important oil/gas bearing segment of the west Lishui sag, filled shallow sea and deltaic deposit which has formed an integrated third order sequence.
古新统明月峰组是丽水西次凹中重要的含油气层段 ,其浅海—三角洲相沉积构成了一个完整的三级层序。
2) the Lishui Sag
丽水凹陷
1.
It is proved by well data that abnormal high-pressure exists widely in the Paleogene Mingyuefeng Formation of the Lishui Sag,the Donghai Basin.
钻井资料证实 ,东海盆地丽水凹陷下第三系明月峰组普遍存在异常高压。
2.
The Tertiary rapid-deposited strata were developed in the Lishui Sag.
丽水凹陷发育第三系快速沉积的地层 ,其重要特点是异常压力非常明显。
3.
An ICP-MS(Inductively Coupled Plasma-Mass Spectrometry) method is used to determine the contents of rare earth element of Paleocene-Eocene samples in the Lishui sag.
采用等离子体质谱分析法测试了东海盆地丽水凹陷古新统砂泥岩样品的稀土元素含量,结果表明,稀土总量在82 2×10-6～182×10-6之间,平均为144×10-6;w(LREE)/w(HREE)比值在4 54～10 02之间,平均为8 67,相对富集LREE;Eu基本为负异常,δEu在0 59～1 03之间,平均为0 73;δCe在0 92～1 09之间,平均为0 98,Ce正常或具微弱的负异常;(w(La)/w(Yb))N在8 23～11 61之间,样品的分布曲线为轻稀土元素富集、重稀土元素亏损型。
3) Lishui sag
丽水凹陷
1.
Carbonate cements and their formation mechanism in Palaeogene sandstones of Lishui sag,East China Sea basin;
东海盆地丽水凹陷古近系储层砂岩中碳酸盐胶结物及形成机制
2.
One Kind of Important Deep-Water Reservoir: The Longitudinal Gravity Currents Sediments——A Case Study in Mingyuefeng Formation in Lishui Sag,East China Sea Basin;
轴向重力流沉积:一种重要的深水储层——以东海盆地丽水凹陷明月峰组为例
3.
Petroleum reservoir filling history and oil-source correlation in the Lishui Sag, East China Sea Basin;
东海盆地丽水凹陷油气源对比与成藏史
4) Xili reservoir
西丽水库
1.
Sedimentation of Xili Reservoir and Its Countermeasures;
西丽水库泥沙问题及对策分析
2.
For the project of vvastewater intercepting and discharge facilities around Xili reservoir.
针对西丽水库环库污水截排工程,截流设施近期采用截流井配合截流堰的方式,远期采用雨污分流方式。
5) Lishui-Jiaojiang sag
丽水-椒江凹陷
1.
The Lishui-Jiaojiang sag locates at Western Taibei depression,the East China Sea Shelf Basin.
丽水-椒江凹陷位于东海陆架盆地台北坳陷西部,其沉降过程经历了裂陷期、坳陷期、抬升期及区域沉降期4个阶段。
6) Lishui Jiaojiang Sag
丽水、椒江凹陷
1.
The Lishui Jiaojiang Sag was a faulted basin developing on the continental margin from the late cretaceous epoch.
丽水、椒江凹陷是晚白垩世以来发展起来的大陆边缘裂陷盆地。
补充资料：凹模壁厚及凹模垫板尺寸
型腔壁部投影面积 壁 厚， 毫 米
F， 厘米2 h1 h2 h3 h4 h5
<5 15~20 30~40 <=10 15~20 30~40
>5~10 20~25 40~50 10~15 20~25 40~55
>10~50 20~30 50~60 15~20 20~30 55~65
>50~100 30~35 60~75 20~25 30~40 65~70
>100~200 35~40 75~85 25~30 40~50 70~75
>200 >40 >85 30~35 50~60 >80
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