论文部分内容阅读
1史密斯地层与非史密斯地层 1．l史密斯地层学的产生、发展与基本原理地层学产生以来的300余年，研究内容基本上属于史密斯地层学（Smith stratigraphy）的范畴。最早的地层学科学奠基人斯坦诺在论文《天然固体中的坚硬物》（1669年）中提出著名的地层学三定律：层序叠加律（Law of Superposition），即若地层未经变动则下老上新；原始连续律（Law of Original Continuity），即若地层未经变动则呈连续体并逐渐尖灭；原始水平律（Law Of Original Horizontality），即若地层未经变动则呈水平或大致水平产状。斯坦诺的三定律第一次把理性带进地层学。
1 Smith Stratum and Non-Smith Stratum 1. Smith’s Stratigraphy Generation, Development, and Fundamentals The 300 years since the foundation of stratigraphy have been studied and are largely within the scope of Smith stratigraphy. The earliest stratigraphic science founder Steinor put forward three well-known laws of stratigraphy in the paper “The Hard Materials in Natural Solids” (1669): Law of Superposition, that is, if the strata were not changed Old and new; Law of Original Continuity, which means continuation and pinch-out if the formation has not changed; Law of Original Horizontality, which is level or general if the formation is unchanged Horizontal production. For the first time, Stein’s three laws bring reason to stratigraphy.