朱红涛;杜远生;何生;

• 1:中国地质大学资源学院
• 2:中国地质大学地球科学学院
• 3:中国地质大学资源学院 武汉430074中国地质大学地球科学学院
• 4:武汉430074

摘要(Abstract)：

模拟层序地层学是层序地层学理论重要的研究手段之一,在国外该项技术较为成熟。层序地层计算机模拟软件采用的算法主要有扩散算法、流体流动算法、几何控制沉积算法、经验数值逼近算法、沉积物搬运的构造校正算法。目前,国外学者对以海平面升降、构造沉降和沉积物供应为主控因素的层序地层概念模拟的适用性提出了质疑,并对层序控制因素的多样性和不确定性进行了深入的研究。结合当前的研究进展,提出了层序控制因素的"多变量系统"观点,将层序的控制因素分为综合变量和独立变量,进一步指出如果假设综合变量为独立变量,则可以简化层序模拟,假设越多,模拟越简单,但模拟结果越粗略;要使模拟结果真实地反映实际地层特征,就要尽可能采用独立变量。

关键词(KeyWords)： 层序地层学;计算机模拟;模拟算法;多变量系统

Abstract:

Keywords:

基金项目(Foundation): 国家自然科学基金项目(40702024)

作者(Author): 朱红涛;杜远生;何生;

Email:

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