- 发源地
- 震源区
- source: n. 1.源头，水源，源泉。 2.根源，本源；来源。 3 ...
- region: n. 1.地方，地域，地带；地区；行政区，管辖区，区；左 ...
- air mass source region: 气团源地
- probable source region: 可能来源区域
- upper mantle source region: 上地幔来源区
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source region中文什么意思
- 发源地
- 震源区
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例句与用法
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- In the term of principles of regional conservational development , to define the area in which we can have estate objection , where concentrate in the area of beikang , nankang , jiuqu and from yuanbaishan to shaoer whose surface area is 5 . 0 km % ( 4 ) in the light of ground water recharge function , the main way to define contents including existing green conservation , water source region conservation is to ecology construct
按照区域保护性开发的原则，界定可适宜进行房地产开发的建设区域，主要集中在北康、南康、九曲及元白山至邵而庄一带，面积约5 . 0km ~ 2 。 ( 4 )根据研究区的主要生态功能：地下水补给功能，研究区内保护重点为现有绿地的保护、水源地的保护。 - In view of the present situation and existential issue of ecological economy of natural forest in diverting water from the south to the north source region , necessities requirement of recover and protection of natural forest are expounded , some basal conditions and favorable factors are analyzed , and policy and suggestions to actualize are advanced
摘要针对南水北调中线水源区天然林的现状和存在的生态经济问题，阐述水源区天然林恢复与保护建设的必要性，分析实施天然林恢复和保护的基础条件和有利因素，提出天然林恢复、保护与生态经济建设实施的政策建议。 - These phenomena show that the fault has strongly activities at the same time . at that time tan - lu fault zone occurred a large - scale left - lateral displacement . the strike - slip movement on the tan - lu fault zone cau sed the zhangbaling uplifting which became source region and the hefei basin appeared strike - slip flexure at the west side of the fault
说明了控盆断裂?郯庐断裂带在该时期具有强烈活动，且以大规模走滑运动为主，郯庐断裂带的走滑使得东侧张八岭进一步快速隆升，仍构成沉积物源系统；在断裂西侧，合肥盆地因走滑而挠曲，形成沉积可容空间。 - Tncyclic diterpanes c20 , c21 and c23 distribution also has relationship with oil gravity , oil and gas production , as well as oil pool formation timing and oil source . rising - patterned oil originates from fengcheng formation , while peak - patterned oil from xiawuerhe formation . four types of migration and accumulation models are put forward : ( l ) fault controlled migration and accumulation along ridge far from source region ; ( 2 ) fault and unconformity controlled migration and accumulation around source region ; ( 3 ) fault controlled migration and accumulation in the slopes within source region ; ( 4 ) biogenetic and low temperature catalyzed gas migration and accumulation in middle and shallow formation
受挤压背景控制，研究区内海西期形成的断裂，全部为逆断裂，活动期长，可以延续到印支期和燕山期，断开层位可以从石炭系上延至诛罗系，它们对区域构造、沉积、油气运聚有显著的控制作用；而燕山期形成的断裂多为小型正断裂，部分为株罗系和白要系内部断裂，部分从徐罗系断至白圣系。 - The time of peak value of low frequency u wind is prior to the peak of rainfall in flood years ; ( 3 ) there are low frequency olr moves northward at low - latitude and southward at mid - latitude at the same time in flood years , the join point is between 20 - 30 n . contrarily , there is n ' t clear confluence area in drought years ; ( 4 ) the source region is about mid - latitude pacific ocean and philippines in flood years and drought years
( 2 )涝年纬向风与olr场的对应关系无论在位相还是在振幅的配置上都比较好，在长江中下游地区降水的峰值出现前期， 20 30 n纬带总是会出现西风峰值，这是与东亚夏季风的北进相联系的；而旱年时，纬向风与olr的主振荡周期总是不一致，两者的配合较差。