吉林大学学报(地球科学版) ›› 2020, Vol. 50 ›› Issue (2): 480-499.doi: 10.13278/j.cnki.jjuese.20190365
方石, 赵云
Fang Shi, Zhao Yun
摘要： 近代沉积学的诸多进步都是由比较沉积学推动的，它对沉积学的发展有重要意义。目前，其被广泛应用于相模式的推断和沉积相带、储层及其非均质性的预测。比较沉积学是利用比较对象所选变量的时空展布建立模型，再利用模型推断预测被比较对象因变量时空展布的沉积学分支学科。它是根据比较沉积学类比原则，在自生旋回、他生旋回识别的基础上开展的或然性推理。完整的比较沉积学工作过程必然存在2个步骤——比较建模和推断预测。其研究方法包括相模式分析法、几何形态分析法、沉积物载荷分散体系分析法和模拟重构法4种，这些方法多与层序地层学方法联合使用。本文根据比较沉积学的原理和方法综合分析了历年来的典型成果。未来比较沉积学将开展更多与边界条件有关的研究、多尺度统一解释的研究，进一步加强量化，提高预测精度的研究。
中图分类号:
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