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1)  tectonic area
构造区
1.
From the geologica aspect of earthquake, and through study on geophysical field, tectonic stress field, geothermal field and fault movement, it is found that high-degree earthquake tectonic area in Bohai area has evident difference with it in Huanghe delta area.
从地震地质角度出发,通过对深部地球物理场、构造应力场、地温场及断裂活动性等方面的研究,发现渤海强震构造区与黄河三角洲在这些方面存在明显的差异,这些差异造成了两个地区在地震活动性方面的差别,渤海更具备发生强震的条件。
2)  structure of mining area
矿区构造
1.
The article introduces the geologic features of deposit in zeolite mining area in Huzhen basin in Jinyun,Zhejiang province from stratums and structure of mining area,magmatic rock in mining area,characteristics of orebody,and features of ore,and summarizes the prospecting signs,which to lay the foundation for research into the characteristics of zeolite deposit and its further application.
从矿区地层、矿区构造、矿区岩浆岩、矿体特征、矿石特征等方面介绍了浙江省缙云县壶镇盆地的沸石矿区矿床地质特征,并总结了找矿标志,为该地沸石矿床的特征及进一步的应用研究奠定了基础。
3)  regional structure
区域构造
1.
Based on the comprehensive research on the geological conditions such as regional structure,formation,depositional reservoirs,features of hydrocarbon source rocks,it is found that the basins in the study area deposits massively thick Cenozoic formation after experiencing rifting period and de.
该区研究程度很低,据现有资料,通过对区域构造、地层、沉积储层、烃源岩特征等石油地质条件的综合研究,认为曾母、北康、南薇西、中建南等盆地经历了断陷期和坳陷期沉积演化后,沉积了巨厚的新生代地层,自下而上发育了冲积扇相、河湖相→滨岸沼泽相→滨海相→浅海相→半深海相沉积体系,区域上存在始新统、渐新统、中新统三套烃源岩,以及渐新统砂岩、中新统生物礁两套主要储层,区域盖层为上新统和更新统浅海—半深海相泥岩。
2.
On the basis of the above division,by integrating the data of regional structure,sedimentary setting,rock observation, core analysis and test, logging and so on,these intervals are determined to be lake regression type delta front sedimentation developed in hot climate.
在此划分的基础上, 结合区域构造、沉积背景、岩心观察、取心分析化验和测井等资料, 确认濮城油田南区沙二上4-7为气候炎热、蒸发强烈、湖面波动大的小型闭塞盆地内发育的湖退式三角洲前缘沉积, 发育有水下分流河道、水下天然堤、水下分流间湾、河口坝、决口扇、远砂坝及滑塌砂体7种沉积微相。
4)  Regional tectonic
区域构造
5)  regional tectonics
区域构造
6)  zone structure
分区构造
1.
Numerical calculation results indicate that the motion parameter of crack propagating speed has little effect itself on zone structure.
数值计算结果表明,运动参量裂纹扩展速度本身对裂尖场的分区构造影响很小。
补充资料:HⅡ区和HⅠ区
      见电离氢区和中性氢区。
  

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