构造层序地层学

阿尔卑斯－亚平宁地区在多年深入工作的基础上形成了系统的造山带地层学研究和地质图表示方法。板块构造学说的诞生使这在７０年代中期初步上升为理论，成为建立地球动力学模型的基础。近年来造山带构造研究的深入和层序地层学发展及这两者的结合导致形成一门新的分支学科：构造层序地层学。它为我国的造山带研究提供了宝贵的经验和新的理论思想。

TECTONIC SEQUENCE STRATIGRAPHY

Based on detailed field survey in area of the Alps and the Apennines, comes into being a systematic method on stratigraphic working and geological mapping in the orogenic belt. The plate tectonics promotes it to raise to the tentative level of theory and become a foundation of establishing geodynamic model in the middle of the 1970s.More recently, the advances of research on the orogenic structures, the developments of sequence stratigraphy, as well as the combination of the both result in a new-formed branch: tectonic sequence stratigraphy. It affords us valuable experience and new theoretical thoughts for work on the orogens in China.