The SDF extracted enzymic methods is yellow.

The article summarizes the present study progress and the application of enzymic hydrolysis for cellulose.

作者就纤维素酶法水解的研究进展及应用作了简要的概述.

To observe the enzymic histochemical and ultrastructural changes of cryopreserved human retina.

观察深低温保存不同时期人视网膜的酶组织化学及超微结构变化.

Enzymic resolution of allethrone in industrial lipase was studied.

研究了工业脂肪酶拆分消旋体烯丙酮醇.

In late Eocene-Oligocene, that is red coarse sediment.

始新世晚期 — 渐新世, 为一套红色粗碎屑沉积.

The unconformity between the Eocene and the Lower Cretaceous is common in Jiuquan basin.

酒泉盆地普遍发育了始新统与下白垩统之间的不整合.

Paleogene Oligocene Linhe formation ( E _ 3 J ) and Eocene Wulate formation ( E _ 2 wl ).

下第三系渐新统临河组 ( E_3l ),始新统乌拉特组 ( E_2wl ).

The funnel-shaped self-potential curve of the Eocene sands is well marked.

始新统砂层的 漏斗形 自然电位曲线形态很明显.

These showed an evolution of increasing diversity through to the Eocene.

一直到始新世,生物多样性都在不断地提高.

It intruded Eocene sandstones.

它侵入始新世砂岩.

Maoxing block saliferous strata are mainly in 4 th Member, Funing Formation , Eocene Series.

茅兴块段含盐系地层主要为始新统阜宁组四段.

There are four hydrocarbon source rocks, Palaeocene, Eocene, Oligocene and Miocene.

西湖凹陷发育古新统 、 始新统 、 渐新统及中新统四大烃源岩系.

Second, it was eroded over 1000 meters during elevating move — ment later Eocene.

其次是区内始新世末期抬升运动,致使始新统及以下老地层受剥蚀,仅始新统最大剥蚀量达1000m, 这是盆地内绝无仅有的.

Non-rewinding: tape will be left positioned where last EOF was written.

不倒带: 到达磁带尾也不回卷,保留在原位.

The state of the stream is revealed by the bad, fail, eof, and good operations.

流的状态由bad 、 fail 、 eof 和good操作提示.

Summarize and file the lesson learnt for each project including NPI & EOL.

总结每个项目在新品导入 和 老项目终结各阶段的经验教训并归档保存.

Objective : To study the treatment mechanic of Er mi ngxiao Oral Liquid ( EOL ) on tinnitus.

目的: 研究耳鸣消口服液治疗耳鸣的机制.

Drive the End of Life procedure in a timely fashion in order to minimize materials exposure.

及时快速驱动产品EOL终止程序,尽可能降低物料闲置.

It is thus held that the eolian Nd input isnegligible to the oceanic Nd budget.

因此,笔者认为风成粉尘对太平洋深水中溶解的Nd总量的影响可以忽略不计.

Occasionally, when mining area occurs in the source area of eolian sand, the indicator element content obviously increases.

Hg则 从粗向细粒级含量逐渐增高,中间变化很小.但在风成沙来源地有矿区存在时, 则出现相应元素的明显升高.

Most loess is considered to be an eolian deposit.

大多数黄土被认为是一种风成沉积.