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This provides constraints that the quartz monzonite granitoid is of the late Yanshanian intrusion, and that the slip structure along the parallel unconformity of the Carboniferous on the Ordovician strata should have occurred no later than ~134 Ma.

测定结果将这些石英二长岩岩枝的侵入时代限定在晚燕山期,并将发育在奥陶系与石炭系平行不整合面之间的构造滑动断层的发育年龄约束在约134 Ma之前。

It has numerousdiastems and/or unconformities in the Ordovician-.

它numerousdiastems和/或不整合于奥陶系,。

In fact, the available sand is insufficient to form a continuous blanket overlying the unconformity

事实上,所补入的砂质物不足以在不整合面上形成连续的盖层。

In fact, the available sand is insufficient to form a continuous blanket overlying the uncon form ity

事实上,所补入的砂质物不足以在不整合面上形成连续的盖层。

The quartz-monzonite porphyry intrusived in the Pre-Ordovician Songduo Group and Carboniferous-Permian Laigu Formation, unconformably covered by the volcanic rocks of Pana Formation.

石英二长斑岩侵入于前奥陶纪松多岩群和石炭-二叠系来姑组中,并被帕那组火山岩呈火山沉积不整合覆盖。

But there are no many tectonic events during this period. From middle Miocene to late Miocene there is a stage of peneplanation in the South China Sea and there are many tectonic events in this area, such as stratum unconformable contact, faults, deformation and magmatism.

而符合南海地区准平原化阶段的时代是在中中新世末至晚中新世(N21/N31)之间,在此时段普遍存在区域构造不整合接触和地层缺失、断裂、变形及火山活动等构造变动事件。

According to drilling, logging and seismic data in the north of the basin, four types of identification signs were determined to the Phanerozoic sequence boundary. And two kinds of sequence boundaries (unconformity and shift surface of deposition) were identified.

应用层序地层学的原理和方法,综合研究盆地北部钻井、测井及地震资料,确定4种层序界面识别标志,在盆地北部新生代始新世—中新世识别出2种类型层序界面:不整合面和沉积作用转换面。

Biyang fault-depression experience three evolutional phase: Mesozoic pull apart, Paleogene rift. Neogene downwarp basins. So it has in turn three basin-fill sequences and responding tectonic sequences, which were specified by regional unconformity; their general sedimentary style respectively is assemblage of fluvial fan~flood lake depositional system, fluvial fan ~ fan delta ~ lacustrine ~ delta depositional system. and fluvial plain ~ sand mudstone flat depositional system.

泌阳断陷历经中生代小型拉分盆地、早第三纪裂陷盆地和晚第三纪坳陷盆地等三个盆地原型的演化、叠合过程,形成了三个盆地充填序列及其所对应的三个构造层序,其界面皆为区域性构造不整合面;沉积总体样式分别为冲积扇~洪水-漫湖沉积体系组合、冲积扇~扇三角洲~湖泊~三角洲沉积体系组合、冲积平原~砂-泥坪~滨浅湖沉积体系组合。

Based on the research of oil geology characteristic of Xing'anling group in Sudeerte area,by researching the three main accumulation factors source rock,transform pathway and trap for oil formation, showed that the main transform pathway for oil migration in K1n are source rock,unconformity and sand body,and trap related with fault is the main place for oil migration.

在苏德尔特地区兴安岭群石油地质特征研究的基础上,对其油成藏的源岩、输导通道和圈闭3个主要成藏要素进行了研究,得到南屯组是其主要源岩,源断裂、不整合面和砂体是油运移的主要输导通道,与断层有关的圈闭是油聚集的主要场所。

Layered described Cambrian - the Triassic formation, with the period of tectonic events on the sedimentary layers and structural features several important period of formation is not integrated interface, and Tajikistan low uplift tectonic evolution into paleouplift a period ( As early as the late Ordovician), paleouplift stereotypes period, the uplift of ancient period (Silurian Period to the Devonian), partial adjustment period in four phases.

分层描述寒武系—三叠系地层,结合各期构造事件研究了各层沉积构造特征及几期重要的地层不整合界面,并将塔中低凸起构造演化分为古隆起形成期、古隆起定型期、古隆起改造期、局部调整期四个阶段。

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