| 沉积盆地热体制研究的基本原理和进展 |
| |
| 引用本文： | 胡圣标.沉积盆地热体制研究的基本原理和进展[J].地学前缘,1995,2(4):171-180. |
| |
| 作者姓名： | 胡圣标 |
| |
| 作者单位： | 中国科学院地质研究所 |
| |
| 摘 要： | 沉积盆地动态热体制研究可以分别在盆地和岩石圈两种尺度上进行，其目的是盆地热历史的重建或恢复。在盆地尺度下，热历史是通过地层中古温标（直接或间接的）反演而获得的；在岩石圈尺度下，则是通过盆地构造热演化模拟正演而获得的。古温标的动力学模型和盆地数学模型是正、反演过程的基础。本文综述了镜质体反射率、磷灰石裂变径迹和蒙脱石－伊利石转化三种主要古地温计的动力学模型和不同类型盆地成因模型的发展概况，勾画了盆地热历史重建正、反演方法程序的基本框架，并就几个相关问题提出了意见。最后介绍了新近开发出的油气盆地热历史及构造热演化模拟系统。
|
| 关 键 词： | 古温标，盆地模型，热历史，构造热演化，热体制，沉积盆地 |
PRINCIPLES AND PROGRESSES ON THERMAL REGIME OF SEDIMENTARY BASINS-AN OVERVIEW |
| |
| Hu Shengbiao,Wang Jiyang.PRINCIPLES AND PROGRESSES ON THERMAL REGIME OF SEDIMENTARY BASINS-AN OVERVIEW[J].Earth Science Frontiers,1995,2(4):171-180. |
| |
| Authors: | Hu Shengbiao Wang Jiyang |
| |
| Abstract: | The dynamic thermal regime of sedimentary basins can be evaluated either onthe basin scale or on the lithosphere scale,which results in reconstruction of the basinthermal history.On the basin scale thermal history is derived from multiple thermal indi-cators by direct or indirect inversion,while on the lithosphere scale it is estimated usingforward modelling of basin tectonothermal evolution,In this paper the progresses in kinet-ic models of three main thermal indicators(R,AFT and I/S)and in basin formation mod-els are reviewed.The inversion and forward models are outlined for reconstruction of thebasin thermal history,and a few of related points are stressed.Finally,a newly developedsimulating system of thermal history and tectonothermal evolution is introduced。 |
| |
| Keywords: | thermal indicators basin model thermal history tectonothermal evolution thermal regime sedimentary basin |
| 本文献已被 CNKI 维普 等数据库收录！ |
