首页 | 本学科首页   官方微博 | 高级检索  
     检索      

磷灰石裂变径迹方法研究沉积盆地古地温—以东营凹陷为例
引用本文:李善鹏,邱楠生.磷灰石裂变径迹方法研究沉积盆地古地温—以东营凹陷为例[J].西南石油大学学报(自然科学版),2003,25(4):4-8.
作者姓名:李善鹏  邱楠生
作者单位:(1.石油大学盆地与油藏研究中心,北京 昌平 102249; 2.长庆油田勘探开发研究院,陕西西安710021)
摘    要:介绍了应用磷灰石裂变径迹(AFTA)方法研究沉积盆地古地温的原理及研究现状,并以东营凹陷的具体数据为例进行了热史反演。研究表明东营凹陷的古地温梯度基本呈降低的趋势以及“马鞍形”的演变特点。从而表明磷灰石裂变径迹研究沉积盆地古地温是一种行之有效的方法,能够为古地温场的研究提供可靠的依据。

关 键 词:磷灰石裂变径迹  古地温  东营凹陷  依据  
收稿时间:2002-12-26

STUDYING THE PALEO-GEOTEMPERATURE OF SEDIMENTARY BASIN BY THE USE OF APATITE FISSION TRACK ANALYSIS:AN EXAMPLE FROM DONGYING DE-PRESSION
LI Shan-peng,QIU Nan-sheng.STUDYING THE PALEO-GEOTEMPERATURE OF SEDIMENTARY BASIN BY THE USE OF APATITE FISSION TRACK ANALYSIS:AN EXAMPLE FROM DONGYING DE-PRESSION[J].Journal of Southwest Petroleum University(Seience & Technology Edition),2003,25(4):4-8.
Authors:LI Shan-peng  QIU Nan-sheng
Institution:(University of Petroleum Beijing 102249,China)
Abstract:This article introduces the theory and present situation of apatite-fission-track-analysis (AFTA) means in studying the paleo-geotemperature of sedimentary basin, and concrete data in Dongying depression is applied to invert the paleo-geotemperature. It can be seen that the paleo-geotemperature gradient in Dongying depression has a descendant trend and an U-shaped evolvement characteristic. It can be seen that the apatite-fission-track-analysis (AFTA) means is an effective way in researching paleo-geotemperature of sedimentary basin. This means can supply reliable basis for the study of paleo-geotemperature field.
Keywords:apatite fission track analysis  paleo-geotemper-ature  study basis  Dongying depression  
点击此处可从《西南石油大学学报(自然科学版)》浏览原始摘要信息
点击此处可从《西南石油大学学报(自然科学版)》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号