Comparar métodos

	Correlación Estratigráfica	Análisis de subsidencia de cuencas
Campo	Geociencias	Geociencias
Familia	Process / pipeline	Process / pipeline
Año de origen	1901	1978
Autor original	Albrecht Penck and Eduard Brückner	McKenzie and Sclater
Tipo	stratigraphic analysis pipeline	tectono-sedimentary analysis pipeline
Fuente seminal	Catuneanu, O. (2002). Sequence Stratigraphy of Clastic Systems. Geological Association of Canada.	Sclater, J. G., & Christie, P. A. F. (1980). Continental stretching: An explanation of the post-mid-Cretaceous subsidence of the Central North Sea Basin. Journal of Geophysical Research, 85(B7), 3711–3739.
Alias	lithostratigraphic correlation, chronostratigraphic correlation, sequence correlation	tectonic subsidence, backstripping, thermal history analysis
Relacionados	5	4
Resumen	Stratigraphic correlation is the practice of identifying equivalent rock layers or chronostratigraphic units across space by tracing physical or chemical signatures. Rooted in 19th-century work on Alpine glacial sequences, this method was formalized in the 20th century by geologists like Vail who unified global sea-level change with depositional sequences. Correlation is foundational to basin-scale understanding of sediment transport, resource distribution, and paleoenvironmental change.	Basin subsidence analysis is the quantitative study of how sedimentary basins deepen over geological time, driven by tectonics, isostasy, and load. Formalized by McKenzie (1978) and Sclater and Christie (1980), this method reveals the mechanical causes of basin development, predicts subsurface temperature and pressure histories, and constrains petroleum generation. Analysis integrates well stratigraphy, seismic geometry, gravity data, and thermal models to reconstruct basin evolution.