Porovnat metody

	Hydrogeologický průzkum	Geologické mapování	Stratigrafická korelace	Analýza vrstev měřených sondou
Obor	Vědy o Zemi	Vědy o Zemi	Vědy o Zemi	Vědy o Zemi
Rodina	Process / pipeline	Process / pipeline	Process / pipeline	Process / pipeline
Rok vzniku	1856	1799	1901	1940s
Tvůrce	Darcy and Theis	William Smith	Albrecht Penck and Eduard Brückner	Guyod and Barnhart
Typ	groundwater systems analysis pipeline	regional geological documentation pipeline	stratigraphic analysis pipeline	subsurface characterization pipeline
Původní zdroj	Fetter, C. W. (2018). Applied Hydrogeology (5th ed.). Prentice Hall.	Compton, R. R. (1962). Manual of Field Geology. John Wiley & Sons.	Catuneanu, O. (2002). Sequence Stratigraphy of Clastic Systems. Geological Association of Canada.	Asquith, G. B., & Gibson, C. R. (2004). Basic Well Log Analysis (2nd ed.). American Association of Petroleum Geologists.
Další názvy	groundwater assessment, hydrogeologic characterization, aquifer mapping	field mapping, geological surveying, lithostratigraphic mapping	lithostratigraphic correlation, chronostratigraphic correlation, sequence correlation	wireline logging, borehole logging, petrophysical analysis
Příbuzné	3	4	5	5
Shrnutí	Hydrogeological survey is the systematic characterization of groundwater systems, including aquifer geometry, water quality, flow paths, and recharge-discharge dynamics. Rooted in Darcy's law (1856) and quantified by Theis (1935), this method is essential for water resource management, contaminant remediation, and hazard assessment. Modern surveys integrate geology, geophysics, geochemistry, and numerical modeling to understand complex subsurface flow systems.	Geologic mapping is the systematic observation and documentation of rock types, structures, and relationships exposed on the land surface. Pioneered by William Smith in 1799, this foundational field method remains essential for understanding subsurface geology, economic geology, hazard assessment, and paleoenvironmental reconstruction. Modern mapping integrates field observations with satellite imagery, digital logs, and GIS technology to create comprehensive three-dimensional geological frameworks.	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.	Well log analysis is the systematic examination of measurements recorded by instruments lowered into a borehole to characterize subsurface lithology, fluid content, and petrophysical properties. Originating in the 1940s, this method has become indispensable for petroleum exploration, groundwater assessment, and engineering geology. Well logs provide direct depth-correlated data that anchor interpretation of seismic surveys and constrain reservoir models.