中生代构造快速沉降的沉积体的楔形展布表明盆地具有前陆岩石圈挠曲成因特征；
The Mesozoic rapid tectonic subsidence and wedge shaped sedimentary bodies indicate the origin of lithospheric flexure in the Chuxiong Basin.
在此基础上，建立了区域中生代构造-流体-成岩成矿地球化学-体化系统模型。
The Mesozoic magmatism and polymetallic mineralization was caused by interaction between deep-derived fluids and Mesozoic multistage tectonic activities.
中国早、晚古生代、中生代和新生代成煤期的大地构造性质，在各个地区可有不同。
The tectonic nature of different regions in China in the Early and Late Paleozoic, Mesozoic and Cenozoic coal-forming periods is different.
新生代构造现象既是中生代时期构造作用的延续，也是始新世以来复杂应力环境作用的结果。
The tectonic phenomena happened in the Cenozoic are caused by both of the continuity of the Mesozoic tectonic processes and the complexity of Cenozoic stress field.
在晚古生代至早中生代，利文斯顿岛中部处于一个独特的浊积扇的构造环境。
The Central Livingston Island was at a special tectonic setting, fan depositional environment, during Late Palaeozoic Early Mesozoic time.
地下热水的形成和分布与断裂构造及中生代花岗质岩浆活动具有密切关系。
The formation, distribution and fault structure of underground thermal water has a close relationship with the Mesozoic granitic magmatic activity.
中生代造山运动造就的山脉和其后由构造隆升形成的高原，也是影响全球气候的主要因素之一。
Mountains produced by the orogenic movement in the Mesozoic time and plateaus formed thereafter by tectonic uplift become an important factor that influences the global climate.
叙述了该地区推覆构造的基本特征及其对中生代陆相红盆的形成、演化过程的控制和改造。
The present paper deals with the basic characteristics of the structures and their control and effect on the formation and evolution of the Mesozoic red continental basin in this area.
加利福尼亚中生代弧-盆-沟系的构造和演化模式一向为世人所重视。
The structural and evolutional model of the Mesozoic are-basin-trench system in California has been attracting the attention.
中生代晚期SE-NW向挤压，奠定煤田构造格架的基础；
The basic framework of coalfield structure was settled under SE-NW directional compression during Late Mesozoic.
湖南省东南部的晚古生代和中生代含煤盆地多处发现推覆构造。
Several nappes have been found in the late Paleozoic and Mesozoic coal-bearing basins in southeastern Hunail.
招—莱地区金矿也是中生代地洼构造岩浆作用成矿的典型例子。
The Jiaodong gold deposit is a typical example of mineralization under the tectonicmagma of Mesozoic geodepression.
太行山造山带被大多数学者称为构造岩浆带，被认为是中生代环太平洋岩浆弧的组成部分。
Taihangshan orogen, called tectonomagmatic belt by most of geologists, is thought to be a part of Mesozoic circum Pacific magmatic arc.
香港地区届华南加里东构造—岩相带南缘，中生代西太平洋岩浆活动带一部分。
Hong Kong special district, located in the south margin of Caledonian tectonic-lithofacies belt, belongs to the part of west Pacific magmatic mobile belt of Mesozoic.
并讨论了龙门山中段中生代前陆盆地的构造演化历史。
The paper also discusses the structural evolution history of the foreland basin in Mesozoic.
地体及其中生代岩浆作用的构造环境是解释这一继承机理的主要因素。
Terrances and their mesozoic tectonic environments of magmatism are the main factor that explains the inheritance mechanism.
等温降压的P-T-t轨迹指示它们很可能是在中生代伸展构造背景下快速抬升到浅部。
P-T-t path of isothermal decompression indicates rapid exhumation history, which was likely related with Mesozoic extension.
鄂尔多斯盆地在中生代晚期存在一期构造热事件。
The Ordos basin on late-Mesozoic exist on a tectonic heat event.
从胡家营的推覆构造可推知汉南地块东南缘北东向构造带，应属于中生代以来所形成的推覆体构造。
It is supposed that the NE structural belt along southeast margin of Hannan Massif belongs to the nappe formed after Mesozoic Era in terms of Hujiaying nappe.
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.
矿床产于中生代花岗闪长岩和古生代钙铝质岩石的接触带中，矿体受构造和岩性控制。
The orebody is located in a contacting belt between granodiorite of Mesozonic and calcareous-aluminous rocks of Peleozoic, and controled by structure and nature of the rocks.
幔源岩浆的底侵及软流圈对地壳的直接加热作用，使上覆地壳发生大规模的岩浆和成矿作用，并导致中国东部中生代时期伸展构造的广泛发育。
The heating from the asthenosphere on the crust subsequently resulted in the intensive magmatism, mineralization, and widespread development of extensional structures in eastern China.
近年来，在浙江多处中生代酸性火山岩中，发现了十分典型、甚具规模的柱状节理构造。
Typical columnar joint structure of considerably large scale found in recent years is distributed in various localities in Mesozoic acidic volcanic rocks in Zhejiang.
中生代左行走滑和早第三纪伸展作用共同控制了渤海海域早第三纪的构造格局。
The Paleogene tectonic framework in Bohai Bay was controlled by both Mesozoic sinistral strike slip and Paleogene extension resulted from diapiric intrusion of mantle.
中生代中晚期的区域构造热事件是太康-济源古生界区域性高热演化形成的主控因素。
The regional tectonicthermal events in the MidLate Mesozoic were the crucial factors controlling the regional high thermal evolution of the Paleozoic in TaikangJiyuan area.
本文是在作者提出的原地重熔模式的基础上，进一步讨论东南地洼区中生代陆壳重熔的大地构造过程以及这一过程所产生的部份区域地质现象。
On the hypothesis of remelting in SITU put forward by the author, this paper discusses both the dynamic process of crustal remelting and the geological effects brought about by the process.
松辽盆地东缘中生代断裂构造十分发育。
Mesozoic faults at the eastern margin of the Songliao Basin were well developed.
在中生代，该盆地的形成与演化受特提斯构造带的控制。
In Mesozoic era, the formation and evolution of the Mesozoic Lanping Simao basin were controlled by the Tethys tectonic zone.
阐述了分布于燕山板内造山带中段的近东西向中生代右行走滑构造系统的几何学与运动学特征。
The geometry and inner structures as well as the kinematics of the east-west dextral strike-slip fault system in the middle segment of the intraplate Yanshan orogenic belt are described.
阐述了分布于燕山板内造山带中段的近东西向中生代右行走滑构造系统的几何学与运动学特征。
The geometry and inner structures as well as the kinematics of the east-west dextral strike-slip fault system in the middle segment of the intraplate Yanshan orogenic belt are described.
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