被动大陆边缘盆地

石炭纪塔里木板块西南缘为离散边缘，形成被动大陆边缘盆地；

The southwestern margin of Tarim basin in Carboniferous was discrete margin , forming passive continental margin basin ;

震旦纪是塔里木盆地被动大陆边缘盆地重要发育期。

Sinian is one of the most important stage of development of passive continental margin basin in Tarim Basin .

中新世，燕山造山运动减弱，导致马更些湾和阿卡帕克（Akpak）阶海侵沉积，该时期为扩散被动大陆边缘盆地。

Middle Miocene , Yanshan orogeny weakened , resulting in the Mackenzie Bay and Acre Parker ( Akpak ), order transgressive deposition , and the period for the diffusion of a passive continental margin basins .

南美洲被动大陆边缘盆地的油气地质特征

Geologic Characteristic of Hydrocarbon in the Passive Continental Marginal Basins of South America

西昆仑地层区发育了被动大陆边缘盆地、俯冲消减带和碰撞造山等三种类型的岩石组合。

But for West Kunlun , there are three types of rock associations of passive continental marginal basin , subduction zone , orogenic belt as well .

珠江口盆地位于中国南海北部，是一个典型的被动大陆边缘盆地；

Pearl River Mouth Basin ( PRMB ) is a typical passive margin basin located on the northern shelf of the South China Sea ( SCS );

对应每一旋回，喀喇昆仑地层区和塔里木地层区发育有被动大陆边缘盆地和碰撞造山两种类型的岩石组合。

For Kala Kunlun and Tarim , two kinds of rock associations , passive continental marginal basin and collision orogenic belt , are developed corresponding to each cycle .

震旦纪到中泥盆世（古亚洲洋阶段或原特提斯洋阶段），盆地经历了陆内裂谷-被动大陆边缘盆地-前陆盆地发展旋回；

During Sinian to Middle Devonian , i.e. the period of paleo-Asian ocean or proto-Tethyan ocean , it experienced the developmental cycle of intracontinental rift-passive epicontinental basin-foreland basin .

层序地层学经过近半个世纪的发展，研究领域由当初的被动大陆边缘盆地扩展到了活动大陆边缘盆地、前陆盆地和陆相盆地；

After the development of about fifty years , the study field of sequence stratigraphy has been expanded from passive continental marginal basin to active continental marginal basin , forland basin and terrestrial basin .

晚泥盆世到三叠纪（古特提斯洋阶段），塔西南边缘经历了陆内裂谷/被动大陆边缘盆地-弧后伸展盆地-弧后前陆盆地发展旋回；

From Late Devonian to Triassic , the period of paleo-Tethyan ocean ocean , the southwestern margin of Tarim experienced the developmental cycle of intracontinental rift / passive epicontinental basin-back-arc extensional basin-back-arc foreland basin .

中新世，盆地南缘发生隆起和侵蚀，导致北极阿拉斯加微型板块后缘变形和广泛不整合发育，该时期至今均为扩散被动大陆边缘盆地。

Miocene , the basin of the southern margin of the uplift and erosion , resulting in Arctic Alaska micro-plate trailing edge deformation and widespread non-integrated development of the period so far are the diffusion of the passive continental margin basin . 2 .

上古生界以前的基底以六安断裂为界，其北为华北板块陆壳型-过渡壳型结晶基底及其上的华北克拉通-被动大陆边缘盆地沉积的上元古-下古生界基底；

The pre-Upper Paleozoic basement is divided by the Liu'an Fault , north of which is crystalline basement of continental and transitional crust of the North China Plate and Neoproterozoic-Lower Paleozoic sedimentary basement formed in the North China Craton and its passive continental margin basin .

北波拿巴盆地及典型被动大陆边缘深水盆地构造演化及层序地层学研究

The Tectonic Evolution and Sequence Stratigraphy Research of Northern Bonaparte Basin and Typical Passive Margins Deep-water Basin

属于被动大陆边缘裂谷盆地的滇黔桂盆地，自加里东运动之后，泥盆纪开始拉开，整个晚古生代延续发展。

The Yunnan-Guizhou-Guangxi basin is a passive continental-margin rift basin . After the Caledonian movement , it began to be pulled apart in the Devonian and continued to develop in the whole of the Late Paleozoic .

西非被动大陆边缘含油气盐盆地构造背景及油气地质特征分析

Tectonic Evolution and Petroleum Geology Characteristics of Petroliferous Salt Basins Area Along Passive Continental Margin , West Africa

莺歌海盆地属南海北部被动大陆边缘新生代高热盆地，其是在古红河断裂带之上发育起来的新生代走滑伸展型盆地，经历了渐新世左旋和上新世右旋的成盆演化过程。

The Yinggehai basin is a young but high geo-temperature basin that was developed in the Cenozoic at the continental margin area of northern South China Sea .

莺歌海盆地是一个在新生代发育起来的南海北部被动大陆边缘的年轻高热盆地，其高地温场及高大地热流值主要集中于盆地中部坳陷区的泥-流体底辟构造带。

The Yinggehai basin is a young but high geotemperature basin that was developed in the Cenozoic at the northern continental margin of South China Sea . Its high geotemperature and heat flow fields are mainly located in the mud-fluid diapir structure areas in the center of the basin .