构造沉降

GPS构造沉降监测数据处理及变形分析

Data processing and preliminary deformation analysis of high precision GPS tectonic subsidence monitoring

对Watts等构造沉降量计算公式的修正

A revision to watts 's formula used to calculate tectonic subsidence

江汉～洞庭湖平原区构造沉降GPS监测的数据处理方法

The data processing in monitoring of structural subsidence in JIANGHAN-DONGTING Lake Plain

TR层序的形成主要是由于层序形成早期的构造沉降和气候起主导作用，其基底快速沉降，湖水供应充分，湖平面快速上升。

Tectonic subsidence and climate dominated the T R sequence in the early period and made the lake level rise quickly .

为了国土资源调查和防洪防灾，在长江中游建立了大地形变GPS监测网，以监测水患区的构造沉降。

In order to investigate land resources and prevent flood and disaster , a GPS geotectonic deformation-monitoring network was established to monitor the tectonic subsidence of the flooded area in the middle reaches of the Changjiang River .

底部层序（SSⅠ）相当于沙河街组三段下亚段，低位体系域不发育，只发育湖侵体系域和高水位体系域，受早期构造沉降和气候控制。

The bottom of sequence ( SSI ) corresponds to the lower submember of Member ⅲ of Shahejie Formation , characterized by lowstand system tracts undeveloped , only lacustrine transgression system tracts and highstand system tracts developed , all of theses are controlled by the early tectonic subsidence and climate .

天津地区构造沉降及控沉远景问题干燥器的顺控风控先行

Tectonic subsidence and prospect of ground subsidence control in Tianjin area

构造沉降的特点影响沉积层序的完整性；

The characteristics of tectonic subsidence also control the perfection of sequences .

河北蔚县煤田构造沉降与构造演化分析

Tectonic Subsidence and Evolution Pattern Analysis in Yuxian Coalfield , Hebei Province

楚雄中生代前陆盆地的构造沉降史研究

Mesozoic tectonic subsidence in the Chuxiong foreland basin , Yunnan

构造沉降过程可划分为7个时期.其中渐新世和中新世为快速构造沉降时期。

The process of tectonic subsidence can be divided into 7 periods .

桂北-桂东加里东期盆地构造沉降史分析

Tectonic subsidence history of the Caledonian basin in Northeast Guangxi

南海曾母盆地新生代晚期构造沉降分析

Analyses of Late Cenozoic Tectonic Subsidence of Zengmu Basin in South China Sea

济阳坳陷中、新生代构造沉降与板块聚敛速率关系探讨

Relationship between Meso-Cenozoic Tectonic Subsidence of the Jiyang Depression and Plate Convergence Rate

沉积环境的演变及主要水流方向，受差异性构造沉降的控制。

While its evolution and flow direction are controlled by differential tectonic subsidence .

第四纪以来构造沉降速率呈加速度增强；

The tectonic subsidence rate has been accelerating since the beginning of the Quaternary ;

试论短周期幕式构造沉降对陆相断陷盆地高频沉积旋回的控制

Control of Short-period Episodic Rifting to Sedimentation of High-frequence Cycle in Continental Rift-subsidence Basin

济阳坳陷新生代构造沉降特征

Characteristics of Cenozoic tectonic subsidence in Jiyang depression

沉积速率和构造沉降是湖泊水深变化的主要控制因素；

The lake level change was mainly controlled by the depositional rate and tectonic subsidence .

区域构造沉降形成规模较大的构造台地、深水阶地和陆坡盆地等；

Tectonic subsidence formed large-scale tectonic mesa , deep water terrace and continental slope basin etc.

琼州海峡北岸西部地区构造沉降分析

An analysis on tectonic subsidence in the west area of the north coast of Qiongzhou Strait

盆地构造沉降和沉积过程主要受北缘和西缘张性断层的控制。

Tectonic subsidence and sedimentation were primarily controlled by the northern and western basin border faults .

进一步分析可见构造沉降比重值的大小与盆地发展演化阶段密切相关。

The values of specific starved subsidence have close relationship to the developed stageS of the basin .

南海万安盆地构造沉降及其油气成藏控制作用

Tectonic subsidence and its control on hydrocarbon resources in the Wan'an Basin in the South China Sea

陆相断陷盆地二级层序时限构造沉降与湖平面变化的响应关系程序优先级中断-由程序进行中断

Lake-level Variation Response to Tectonic Subsidence in a Second-Order Sequence of Continental Rift Basin software priority interrupt

层序地层的主控因素包括全球海平面变化、构造沉降、气候、物源供给等方面，在不同性质的盆地内它们所起的作用大小不一，在前陆盆地中以构造沉降控制为主。

The sequence stratigraphy is mainly controlled by the eustatic fluctuation , tectonic subsidence , climate and provenance .

构造沉降和沉积物供给因素对层序控制作用的转换促使其形成层序和体系域的边界。

The change of the controlling factors caused the formation of the boundaries of sequences and system tracts .

沉积和层序特征受到海平面变化、构造沉降和碳酸盐沉积速度的共同控制。

The sedimentary and sequence characteristics are influenced by sea-level fluctuation , tectonic subsidence and sedimentary rate of carbonate .

古近纪时期构造沉降速率显示出快速沉降特征主要由断层的强烈活动所致。

Tectonic subsidence rate show the character of the rapid subsidence which is leaded by the activity fault in Paleogene .

层序发育的影响因素可分为构造沉降、沉积物供给和气候因素。

The development of sequence can be controlled by three factors , namely tectonic subsidence , sediment supply and climate .