1) terrestrial stratotype
陆相层型
1.
Theory, methods and urgency of establishing the terrestrial stratotype are discussed based on the study of the stratotype candidate of terrestrial Jurassic-Cretaceous boundary, Luanping, northern Hebei Province, compared with "Revised Guidelines" of the ICS and stipulation of the International Stratigraphic Guide.
从总结陆相侏罗-白垩纪地层界线的研究成果和工作方法入手，结合国际地层委员会“修订准则”和国际地层指南的规定，论述了建立“陆相层型”的紧迫性、理论和方法。
2) continental sequence
陆相层序
1.
The transgressive systems tract of the continental sequences in the Biyang fault depression:oil and gas geological significance;
试论泌阳断陷陆相层序水进体系域的油气地质意义
2.
Mechanism of allowable space change and its diagram in continental sequence, upper member of He-3, Paleogene, Biyang depression.;
泌阳断陷下第三系核三上段陆相层序可容空间变化机理及其图解
3.
The sedimentary base\|level cycle changes could control the formation and evolution of continental sequence stratigraphy, and act as reference framework for the prediction of reservoirs.
沉积基准面旋回变化控制着陆相层序地层的形成与演化 ,并为预测陆相储层的发育与展布提供了一个参照格架。
3) terrigenous sequence
陆相层序
1.
Lithologic geochemical cyclicity in terrigenous sequence of the upper member of Eh3 in Shuanghe Zhaoao, Biyang fault depression;
试论泌阳断陷双河-赵凹地区下第三系核三上段陆相层序中岩石地球化学旋回性特征
2.
The oil distribution rule of oil and gas in the Tertiary basin of Chaidamu was studied by using the model of the terrigenous sequence.
应用陆相层序地层概念模型 ,研究柴达木第三纪盆地层序格架中油气分布规律 ,探讨各层序中不同体系域中沉积体系的配置关系、生储盖组合、油气聚集模式、圈闭类型及分布。
3.
A complete terrigenous sequence in faultdepreesed lacustrine basin can be divi ded into four system tract: Lowstand System Tract (LST), Trangressive System Tra ct (TST), Highstand System Tract (HST) and Regressive System Tract (RST), which has typical geometrical configuration and respectively consists of lowstandagg radation regression, highstandaggradation and progradation.
断陷湖盆中一个完整陆相层序的体系域具四分性，即低水位体系域（ＬＳＴ）、水进体系域（ＴＳＴ）、高水位体系域（ＨＳＴ）及水退体系域（ＲＳＴ），该四分体系域具显著的几何构型特征，它们分别由低位加积小层序组、退积小层序组、高位加积小层序组及进积小层序组构成。
4) continental reservoir
陆相储层
1.
The research of microcosmic mechanism and geologic origin of low-resistivity layers in continental reservoir of Jiyang Depression showed that microcosmic factors for reducing apparent resistivity of oil layer included mainly high-salinity formation water of reservoir,additive conductivity of shale in reservoir and development of fine pores of reservoir.
对济阳坳陷陆相储层低电阻率油层的微观形成机理及地质成因的研究表明,引起油层视电阻率降低的微观因素主要有:①储层含高矿化度的地层水;②储层所含粘土的附加导电;③储层微孔隙发育。
5) continental strata
陆相地层
1.
Lateral aggradation of continental strata is widely developed,resulting in highly variable litholo-gies and lithofacies.
陆相地层侧向加积作用广泛发育,导致岩性、岩相多变。
6) Continental Redbeds
陆相红层
1.
Studying the Continental Redbeds of Yaojia formation,we come to a conclusion that redbeds can lies in underwater environments and summarize the area and thickness of the Redbeds of Yaojia formation that lies main in Sanzhao depression and Chaoyanggou rank and lesser in Qijia-Gulong depression.
通过对姚家组陆相红层的研究,突破了以往见到红层就划分为水上环境的认识,总结了姚家组红层的分布范围和厚度特征,其主要分布在三肇凹陷和朝阳沟阶地,在齐家-古龙凹陷也有一定分布。
补充资料：层积型电子照相感光体
分子式：
CAS号：
性质：由电荷产生层(CGL；charge carrier generation layer)和电荷转移层(CTL；charge carrier transport layer)层积组成的静电复印感光体。通常，在支撑体(如聚酯膜)镀铝导电层基板上涂以CGL(由电荷产生材料和少量树脂组成的，厚度一般为0.1～0.4μm)，然后再涂上CTL(由电荷转移材料和聚碳酸酯等树脂组成，厚度一般为5～30μm)，感光体受电晕放电处理之后，表面上充满了均匀的电荷(正电荷或负电荷)，受到光照时，CGL中的电荷产生材料分子形成电荷载流子，如果感光体表面带负电荷，则空穴通过CTL中的电荷转移材料分子传递到表面与负电荷中和，使光照部位的电荷消失。如果感光体表面带正电，则电子通过CTL传递到表面与正电荷中和。未照光的部位保留着感光体表面的电荷，形成了静电潜影。当它和带有相反电荷的静电色粉接触后就能形成影像，将色粉的影像转印到纸上，再经热处理即得到复印件。
CAS号：
性质：由电荷产生层(CGL；charge carrier generation layer)和电荷转移层(CTL；charge carrier transport layer)层积组成的静电复印感光体。通常，在支撑体(如聚酯膜)镀铝导电层基板上涂以CGL(由电荷产生材料和少量树脂组成的，厚度一般为0.1～0.4μm)，然后再涂上CTL(由电荷转移材料和聚碳酸酯等树脂组成，厚度一般为5～30μm)，感光体受电晕放电处理之后，表面上充满了均匀的电荷(正电荷或负电荷)，受到光照时，CGL中的电荷产生材料分子形成电荷载流子，如果感光体表面带负电荷，则空穴通过CTL中的电荷转移材料分子传递到表面与负电荷中和，使光照部位的电荷消失。如果感光体表面带正电，则电子通过CTL传递到表面与正电荷中和。未照光的部位保留着感光体表面的电荷，形成了静电潜影。当它和带有相反电荷的静电色粉接触后就能形成影像，将色粉的影像转印到纸上，再经热处理即得到复印件。
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