在利用地震层位构造图编制盆地区域性等厚图时，可以用断层面的残留厚度来描绘断层在平面上的分布。
In compiling areal isopach of a basin from seismic horizon structure map, we can use the residual thickness at both sides of fault plane to show the horizontal distribution of a fault.
对中国海域中生代盆地地质特征进行了分析，认为海域中生代盆地主要有构造残留型和断陷型两类。
From geological features of Mesozoic basins in offshore China, they are divided into two types: residual structure basin and fault basin.
这一沉积记录所反映的演化趋可能标志着古特提斯残留海的一次重大构造转折。
The evolutionary tendance reflected by the above sedimentary record probably signifies an important tectonic turn in the history of the residual Paleotethys ocean.
经晚白垩世和新近纪的构造反转改造后，呈改造残留型含油气、含煤盆地。
After reverse tectonic period in Late Cretaceous and Neogene, it became a relict basin with oil-gas and coal.
湖泊分类：构造湖、火山口湖、冲积残留湖、堰塞湖、冰川湖、喀斯特湖、风成湖、陨石撞击湖和人工湖。
Types of lakes: tectonic lake, crater lake, fluvial lake, dammed lake, glacier lake, karst lake, Aeolian lake, impact crater lake and artificial lake.
通过深入揭示残留地层所蕴涵的构造信息，为正确认识渤海湾盆地新生代形成演化机制提供了新的依据。
Through deep revealment of the geological information, new evidence was obtained for a correct recognition of the Cenozoic forming and evolution mechanism of Bohai Bay Basin.
已知金矿床的形成与分布均与韧性剪切带有关，韧性剪切带是形成绿岩型金矿的主要控矿构造。强烈韧性变形和破碎并富含绿岩带残留体的TTG岩系与金成矿关系密切。
The formation and distribution of the known gold deposits are both related to ductile shear belts, which are major ore-controlling structure of greenstone type gold deposits.
前新生代盆地结构、残留厚度与基底三分性特征均表现出受深部断裂构造的影响和控制。
Pre-Cenozoic basin structure, residual thickness and trichotomous property of basement are all shown by the impact and control of deep faults.
前新生代盆地结构、残留厚度与基底三分性特征均表现出受深部断裂构造的影响和控制。
Pre-Cenozoic basin structure, residual thickness and trichotomous property of basement are all shown by the impact and control of deep faults.
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