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造山带层序地层
相关语句
  orogenic sequence stratigraphic
     THE OROGENIC SEQUENCE STRATIGRAPHIC TYPES AND THEIR CONTROLLING FACTOR TAKING THE TRIASSIC OF EASTERN KUNLUN AS EXAMPLE
     试论造山带层序地层的类型、特点和控制因素——以东昆仑三叠系为例
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  “造山带层序地层”译为未确定词的双语例句
     We can not use the model of the sequence stratigraphy of the stable area for that of the orogenic zone and it is necessary to establish the model of the fluctuation of sea level controlled by different tectonic environments.
     从而对造山带层序地层不能套用稳定地区的层序地层模式,而需要从自身特征出发,因地制宜,建立起不同构造环境控制下的海平面变化模式。
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  相似匹配句对
     SEQUENCE STRATIGRAPHIC CHARACTERISTICS OF SICHUAN BASIN
     四川盆地层序地层特征
短句来源
     A DISSCUSION ABOUT THE STRATIGRAPHIC DIVISION IN OROGENIC BELT
     浅谈造山带地层划分
短句来源
     STRATUM
     地层
短句来源
     CHARACTERISTICS OF NON SMITH SEQUENCE OF EAST JUNGGAR OROGENIC BELT
     东准噶尔造山带东部非史密斯地层层序特征
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     ON SEQUENTIAL STRATIGRAPHY PATTERN
     层序地层模式浅析
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Sequence stratigraphy has been developed in China for nearly 20 years. By the hard work of Chinese geologists, it went through three development stages which are beginning, high-speed development and mature development. Among the stages the Chinese geologists progressed quite a lot and acquired plentiful achievements especially in the research of regional sequence stratigraphy, theoretical sequence stratigraphy, sequence stratigraphy with mineral controlling, sequence stratigraphy in oil and gas exploration,...

Sequence stratigraphy has been developed in China for nearly 20 years. By the hard work of Chinese geologists, it went through three development stages which are beginning, high-speed development and mature development. Among the stages the Chinese geologists progressed quite a lot and acquired plentiful achievements especially in the research of regional sequence stratigraphy, theoretical sequence stratigraphy, sequence stratigraphy with mineral controlling, sequence stratigraphy in oil and gas exploration, high-resolution sequence stratigraphy, Milankovitch cycles, continental sequence stratigraphy (including alluvial system and desert aeolian system), applications of new techniques and methods in sequence stratigraphy (seism, well-log, computer simulation, neutron technique, cosmogenic nuclide etc.), dynamic sequence stratigraphy in basin depression and mountain building, sequence stratigraphy in the Tibet plateau and orogenic zones, diagenetic sequence stratigraphy, chemical sequence stratigraphy, tectonic sequence stratigraphy and sequence-lithofacies palaeogeography mapping etc. Based on the analysis of research status of Chinese sequence stratigraphy, it is suggested that Chinese geologist should enhance the application of sequence stratigraphy, and also should pay more attention to the basis research, technique improvement and feature development, in order to devote themselves to the development of sequence stratigraphy.

层序地层学在中国已经近 2 0年 ,通过中国地质学家的努力下 ,层序地层学的发展可以分为 :萌芽阶段 ,快速发展阶段 ,成熟发展阶段。在中国区域层序地层研究、在层序地层理论体系、层序地层与矿产控制作用、层序地层与油气勘探、高分辨层序地层和米兰柯维奇旋回及米级旋回层序地层、陆相层序地层 (包括冲积体系和沙漠体系 )、新技术、新方法在层序地层中的应用 (包括地震、测井、计算机模拟、中子技术、宇宙核素等 )、盆山转换和动力层序地层、青藏高原层序地层及造山带层序地层、成岩层序地层和化学层序地层、构造层序地层、层序地层岩相古地理编图等各个方面都有很大发展 ,取得了丰硕的成果。在中国层序地层学研究状况分析基础上 ,提出中国层序地层学应该在加强应用 ,重视基础 ,提高技术 ,发展特色等四个方面努力创新 ,为层序地层学科的发展贡献中国地质学家的力量。

Based on the Triassic of Eastern Kunlun, the area far from the orogenic core zone possesses the potential for studying the sequence stratigraphy. However, the sequence strata there are clearly different from the craton in the following aspects:1) System tract is not complete; 2) condensed member is lacking; 3) Fluctuation of sea-level of the orogenic zone remains sharply wavering throughout.Thus the factors controlling the fluctuation of sea-level of the orogenic zone and sequence stratigraphy are not the global...

Based on the Triassic of Eastern Kunlun, the area far from the orogenic core zone possesses the potential for studying the sequence stratigraphy. However, the sequence strata there are clearly different from the craton in the following aspects:1) System tract is not complete; 2) condensed member is lacking; 3) Fluctuation of sea-level of the orogenic zone remains sharply wavering throughout.Thus the factors controlling the fluctuation of sea-level of the orogenic zone and sequence stratigraphy are not the global eustatic fluctuation but are the regional tectonic process and the provenance control. We can not use the model of the sequence stratigraphy of the stable area for that of the orogenic zone and it is necessary to establish the model of the fluctuation of sea level controlled by different tectonic environments.

造山带地区的层序地层往往被视为禁区,以东昆仑三叠系为例,认为造山带除核部外,远离造山带核部地区基本具备了开展层序地层研究的条件,但造山带层序地层与克拉通相比具显著的不同:1)体系域的不完整;2)凝缩段常常缺乏;3)造山带海平面变化特征自始至终呈现剧烈的跳跃式。因而控制造山带海平面变化和层序地层的并不是全球海平面变化,而是区域构造作用和物源控制。从而对造山带层序地层不能套用稳定地区的层序地层模式,而需要从自身特征出发,因地制宜,建立起不同构造环境控制下的海平面变化模式。

 
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