晚成 meaning in English
altricial
Examples
- The strata of es , to middle ed3 belong to sequence i and upper ed3 to ed , to sequence ii . ( 2 )
( 2 )埕岛东斜坡地区东三段至沙一段的沉积砂体成岩作用阶段基本已进入晚成岩a 、 b期。 - Abnormal evolution of shallow reservoirs has related to the upward movement of hot fluid . influenced by the upward movement of hot fluid , shallow reservoirs have shown the characters of late diagenetic stage b ( or a )
浅层气藏储层异常演化特征与泥底辟活动及热流体上侵有关，热流体侵入促使浅部储层提前进入晚成岩阶段b期(或a期) 。 - For we know only of the “ late bloomers ” who have eventually come to bloom at all ; we don ' t know the potential late bloomers who , cut off from support and response in their youth , never manage to come into their own at all
我们只知道那些最终有所成就的“大器晚成者” ；然而我们却不知道那些在幼年失去支持和关注的潜在的“晚成者”最终未能成功。 - The creation of an association compiled of professional colleagues for a common purpose f . resolution of conflicts much be accomplished by all colleagues working together this study reveals the results of the education department , the principal and teacher and a variety of educators who have provided very valuable data for this project
革新及具有凝讼力f曹闲题出现晚成灵均原惫解泱本研究报扒研究结果，封教育主管部闩、校畏及教句堤供相阴意兄。 - The variations in trace element contents and ratios may hold up a mirror to the lake - level fluctuations and climatic changes , which , in turn , have exerted a direct and important effect on the sequence stratigraphic development . collectively , the reservoir rocks from the yanchang formation consist dominantly of the delta front subfacies subaqueous distributary channel and channel - mouth bar microfacies and delta plain subfacies subaerial distributary channel microfacies fine - grained feldspar sandstones and siltstones . the reservoir rocks have been subjected to three stages of diagenetic and porosity evolution : ( 1 ) the porosity reduction by the mechanical compaction and chemical pressure solution during the early diagenetic stage ; ( 2 ) the porosity increase by the dissolution during the a substage of the late diagenetic stage , and ( 3 ) the porosity reduction by the cementation and filling during the b substage of the late diagenetic stage
系统的储层特征研究表明，该区延长组储层成因类型主要为三角洲前缘水下分流河道、河口砂坝及三角洲平原水上分流河道微相细粒长石砂岩、粉砂岩；储层岩石经历了压实，胶结，溶蚀等成岩作用，历经早成岩机械压实和化学压溶孔隙缩小期、晚成岩a亚期溶蚀作用孔隙扩大期及晚成岩a亚期( b亚期)胶结充填孔隙缩小期三个成岩-孔隙演化阶段；储层物性总体上具有较低孔渗、低孔渗的特点，孔隙类型主要为粒间溶孔、残余粒间孔隙、粒内溶孔、晶间孔及晶间溶孔，裂缝不发育，储集岩排驱压力和中值压力较高，孔隙结构类型以细小孔-微孔隙，微细喉-微喉型为主。