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permian stratigraphic
相关语句
  二叠系地层
     In the paper the authors discuss the stratigraphic division of the Permian and age assignment of the Permian stratigraphic units in the Sonid Left Banner area. It is considered that the Permian in the area should comprise the Dashizhai Formation, the Zhesi Formation and the base of the Linxi Formation.
     探讨了苏尼特左旗地区二叠系地层单元的划分与时代归属,认为该区二叠系地层应包含大石寨组,哲斯组与林西组底部,重新厘定了该区二叠系剖面序列。
短句来源
  “permian stratigraphic”译为未确定词的双语例句
     The Study on Carboniferous and Permian Stratigraphic Characteristics and Distribution in Jiyang Depression of Shandong
     山东济阳坳陷石炭、二叠纪地层特征与分布研究
短句来源
     It is considered that the sequence here should be ascribed to the Late Permian stratigraphic system of the southern Junggar basin,moreover,the above two can be well contrasted. This study may provide some new information on the comprehensive evaluation of the oil and gas in the Turpan-Hami basin,espcially on the regarding of the Upper Permian as an important prospecting target,and going a deep further to find oil and gas resources.
     认为这里的晚二叠世地层与准噶尔盆地南缘上二叠统完全可以对比,应采用统一的地层名称,这对于吐哈盆地油气资源的综合评价,特别是把上二叠统作为重要的勘探目的层,向更深层次寻找油气资源提供了新的资料。
短句来源
     The development of the Late Permian Dibuco Formation has been checked and verified and the original Middle Jurassic Dawaxung Group is redefined as Permian strata, thus improving and enriching the Permian stratigraphic system.
     查证测区内发育晚二叠世敌布错组,将原中侏罗世达雄群修定为二叠纪地层,完善与丰富了二叠纪地层系统。
短句来源
     The crustal components in the region include: late Archean crystallization basement, middle-late Proterozoic fold series and Paleozoic cover of upper Sinian to Permian stratigraphic system.
     区域地壳结构有基底结晶岩系(新太古界)和褶皱岩系(中新元古界),盖层为古生界,自上震旦统至二叠系基本连续出露。
短句来源
  相似匹配句对
     PERMIAN PALEOFLORA AND STRATIGRAPHIC SUBDIVISION IN CHINA
     中国二叠纪植物群与地层分区的关系
短句来源
     On event stratigraphic markers of the Permian-Triassic boundary
     二叠系-三叠系界线的事件地层学标志
短句来源
     Permian Period
     二迭纪
短句来源
     ON STRATIGRAPHIC CLASSIFICATION
     试论地层单位的划分
短句来源
     On the Carboniferous-Permian boundary
     论石炭系与二叠系的分界
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The Lamellibranchiate fossils firstly discovered in the upper part of Jijicao Group of Zhaobishan in Shanshan of Xinjiang have been systematically studied in this paper,accompanied with a thorough discussion on fossil assemblages and their ages.The Late Permian sequence along the margin of south Bogda Mt.has been reconstructed with profile of fossils assemblage,lithology and sedimentary characteristics,as well as structure of the sections.It is considered that the sequence here should be ascribed to the...

The Lamellibranchiate fossils firstly discovered in the upper part of Jijicao Group of Zhaobishan in Shanshan of Xinjiang have been systematically studied in this paper,accompanied with a thorough discussion on fossil assemblages and their ages.The Late Permian sequence along the margin of south Bogda Mt.has been reconstructed with profile of fossils assemblage,lithology and sedimentary characteristics,as well as structure of the sections.It is considered that the sequence here should be ascribed to the Late Permian stratigraphic system of the southern Junggar basin,moreover,the above two can be well contrasted.This study may provide some new information on the comprehensive evaluation of the oil and gas in the Turpan-Hami basin,espcially on the regarding of the Upper Permian as an important prospecting target,and going a deep further to find oil and gas resources.

系统研究了首次发现于新缰鄯善照壁山上芨芨槽群上部的瓣鳃动物化石,讨论了化石组合特点及地质时代。根据化石组合特点、岩性和沉积特证,以及剖面结构,重新厘定了博格达山南缘晚二叠世地层层序。认为这里的晚二叠世地层与准噶尔盆地南缘上二叠统完全可以对比,应采用统一的地层名称,这对于吐哈盆地油气资源的综合评价,特别是把上二叠统作为重要的勘探目的层,向更深层次寻找油气资源提供了新的资料。

In the paper the authors discuss the stratigraphic division of the Permian and age assignment of the Permian stratigraphic units in the Sonid Left Banner area. It is considered that the Permian in the area should comprise the Dashizhai Formation, the Zhesi Formation and the base of the Linxi Formation. The authors revise the sequence of the Permian section of the area. On the basis of an analysis of the chemical composition and REE abundances of the volcanic rocks in the Dashizhai...

In the paper the authors discuss the stratigraphic division of the Permian and age assignment of the Permian stratigraphic units in the Sonid Left Banner area. It is considered that the Permian in the area should comprise the Dashizhai Formation, the Zhesi Formation and the base of the Linxi Formation. The authors revise the sequence of the Permian section of the area. On the basis of an analysis of the chemical composition and REE abundances of the volcanic rocks in the Dashizhai Formation, it is considered that this formation was tectonically located on the active continental margins and that the time for the final convergence between the Sino Korean plate and Siberian plate should be middle Early Permian.

探讨了苏尼特左旗地区二叠系地层单元的划分与时代归属,认为该区二叠系地层应包含大石寨组,哲斯组与林西组底部,重新厘定了该区二叠系剖面序列。通过对大石寨组火山岩岩石化学、稀土元素的分析,认为大石寨组所处的大地构造环境为活动大陆边缘,中朝板块与西伯利亚板块的最终汇聚时期应为早二叠世中期。

Late Permian stratigraphic, sedimentary and paleotectonic studies along a corridor profile across the Yangtze paleocontinent and its southern margin reveal the sedimentary evolution, subdivide the depositional sequences, and reconstruct the stratigraphic framework based on lateral correlation and tracing of the bounding surfaces and depositional systems. This corridor profile transects the Yangtze craton and a molasse sag zone in its southern margin. It is demonstrated that the Late Permian...

Late Permian stratigraphic, sedimentary and paleotectonic studies along a corridor profile across the Yangtze paleocontinent and its southern margin reveal the sedimentary evolution, subdivide the depositional sequences, and reconstruct the stratigraphic framework based on lateral correlation and tracing of the bounding surfaces and depositional systems. This corridor profile transects the Yangtze craton and a molasse sag zone in its southern margin. It is demonstrated that the Late Permian sedimentary evolution along the investigated profile evidently resulted from the interplay of sea level change, differential subsidence and sediment supply within the given tectonic units. In the cratonic interior, high frequency sea level fluctuation exerts an important control on the formation of the third order and fourth order sequences, and is the basis for transfacies correlation. The evolution of sequence succession in the taphrogenic zone is so much affected by the intense tectonic subsidence that it is hardly correlatable to that in the cratonic interior.

INTRODUCTIONTheconceptsandterminologyofmodernsequencestratigraphyoriginatedfromseismicstratigraphylinkedtopetroleumandgasexpl...

 
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