剥蚀厚度估算是进行古构造特征研究、烃源岩热演化史模拟和古流体势分析的重要基础工作。
The estimation of erosion thickness is a foundation for studying palaeostructural characteristic, modeling source rock thermal evolution history and analyzing palaeo-fluid potential.
礁分布可能受隐伏基底断裂活动所形成的古构造控制。
Reef distribution may be controlled by the paleostructure produced by the activities of buried basement faults.
石炭系印支期的古构造高部位是埋藏溶解孔发育的有利地区。
The palaeostructure high part of Carboniferous in Indosinian epoch is favourable to the development of burial corrasion pores.
古构造恢复是探索多旋回盆地油气藏改造、重组的有效手段之一。
Paleostructure restoration can be treated as one of the practical ways for understanding manners of hydrocarbon reservoir reformation and rearrangement in multi-cycle evolved basins.
盆地覆盖区古构造应力场分析一直是盆地动力学研究的一个难题。
The analysis of the paleotectonic stress field in the overburden of a basin is always a difficult problem in basin dynamic research.
古构造格局和生烃中心可能是导致不同地区成藏时间差异的主要原因之一。
The palaeo structural framework and the distribution of hydrocarbon supply center might be one of the key controlling factors for the difference in accumulation times within different areas.
本文提出了碳酸盐岩裂缝性储层的一种新评价方法——古构造应力场数值模拟法。
This paper presented an evaluation method of carbonate fractured reservoirs, which is a numerical simulation method for the an ciend structural stress field.
松树沟逆冲推覆构造研究对恢复蛇绿岩组合层序及其古构造环境具有重要的地质意义。
Studing the thrust-nappe help us to re-establish the Songshugou ophiolite sequence and its ancient tectonic environment.
从构造模拟目标、构造模型建立、构造模拟三个方面探讨了古构造应力场数值模拟的方法。
This paper analyses the numerical simulation method for Paleo-tectonic Stress Field from three aspects, namely tectonic simulation target, building of the tectonic model and tectonic modeling.
对研究区中、晚石炭世区域古构造环境的认识，目前存在有限洋盆、裂陷槽、裂谷、岛弧之争。
There are many disputations about the geological setting in Carboniferous of the Bogeda Mountain, such as small oceanic basin, aulacogen, rift or Island-Arc and so on.
笔者讨论了其术语、岩块、基质特征、形成机制和古地理古构造条件，并列表分析了它与混杂堆积的区别。
The relevant terminology, block and matrix characteristics, genetic mechanism, palaeogeography and tectonics are discussed in this paper together with their distinction from melanges.
在几乎所有有关东南亚的古构造再造中，人们普遍认为从泰国到马来西亚半岛存在着一条或多条长缝合带。
The existence of one or more long suture zones extending from Thailand to Peninsular Malaysia has been widely accepted in almost all the palaeotectonic reconstruction of Southeast Asia.
在琼库恰克构造带的形成和发展过程中经历了海西运动期古构造形成阶段及喜马拉雅运动期现今构造定型阶段。
The formation and development of Qongkuqak structural zone underwent two stages, i. e. , Hercynian paleostructural forming stage and Himalayan present-structural forming stage.
研究认为：多旋回的演化历史、古构造格局、构造变形特征及重要的侵蚀间断对油气藏的形成与分布有明显的控制作用。
The multicycle evolutional history, paleostructural configurations. structural characteristics and major erosional unconformities control the generation and distribution of oil and gas reservoirs.
江苏下扬子区的海相中—古生界构造演化经历了前扬子板块、稳定地台和西太平洋活动陆缘等三大阶段。
Marine Meso-Paleozoic structures in the region have undergone three evolution stages of Pre-Yangzi Plate, stable platform and West Pacific active continental margin.
构造运动造就的古地貌在陆相盆地，特别是裂谷盆地对层序形成与发育起着重要的控制作用。
Paleo morphology resulted from tectonic movement controlled the sequence formation and development of continental basins, especially of rift basins.
这样高的古地温梯度肯定与构造热事件有关。
济阳坳陷“古潜山”圈闭体系按二级构造带可划分为高潜山油气藏体系、中潜山油气藏体系和低潜山油气藏体系。
"Buried hill" trap system of Jiyang depression can be divided into high, medium and low reservoir system of buried hill according to secondary structure.
古近纪末期逆冲构造形成机制与印度板块向欧亚板块之下俯冲的远程效应有关。
The formation mechanism of thrust tectonics in the Paleogene was supposed to be related to a far field effect caused by collision between the Indian and the Eurasian plates.
构造活动主要通过对沉积古地貌的控制而控制着沉积物的分布及沉积物本身的特征。
Structure activity controlled the distribution and characteristics of sediments by controlling the palaeogeomorphology of sedimentation.
矿化受古岩溶构造及具多期活动的NE -NNE向断裂控制。
The mineralization is controlled by ancient karst structure and the NE-NNE oriented faults characterized by multi-stage activity.
本文通过对六苴铜矿床的矿床地质特征分析，认为控矿因素可归结为下列几个方面：层位、岩性、构造、岩相、古地理等。
According to the geological characteristics of Liuju copper deposits, the controlling ore-forming factors include stratigraphy, lithology, structure, lithofacies and paleogeography.
本文从古台山—高家坳金矿带北西向构造入手，总结其控矿特征，指出找矿方向。
Starting to study from NW-trending structure of Gutaishan-Gaojiaao gold deposit zone, in this paper, deposit-controlled characteristic is summarized and prospecting orientation is pointed out.
负反转构造是断块型古潜山形成的主要因素，其构造演化决定了断块型古潜山的形成。
Negative reversal structures are the main factors of forming fault - block type buried hills and their structural evolution determined forming the fault - block type buried hills.
以上认识为中、越交界地区构造上属古特提斯造山带提供了新证据，为重塑该地的古特提斯演化提供了重要资料。
The knowledge provides new testimonies for the area bordering China and Vietnam being, tectonically, Paleotethysides and key data for reconstructing Paleotethyan evolution there.
全球性旋回沉积是全球海平面变化、全球气候条件、全球构造演化、全球古地理背景及沉积特征综合作用的产物。
Cyclic deposition on a global scale is the product of the changes in sea-level, tectonics, climate, geography and depositional features of the global or the combination of these.
构造地质背景与新构造运动控制着长江三角洲沉积盆地的演化，影响着古地理环境与沉积格局。
The neotectonics controls the evolution of the sediment basin, paleo - depositional environment and pattern of the present Changjiang delta plain.
构造地质背景与新构造运动控制着长江三角洲沉积盆地的演化，影响着古地理环境与沉积格局。
The neotectonics controls the evolution of the sediment basin, paleo - depositional environment and pattern of the present Changjiang delta plain.
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