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Abstract Decoding the complete history of Earth and our solar system requires the placing of the scattered pages of Earth history in a precise chronological order, and the 40 Ar/ 39 Ar dating technique is one of the most trusted dating techniques to do that. The 40 Ar/ 39 Ar method has been in use for more than 40 years, and has constantly evolved since then. The steady improvement of the technique is largely due to a better understanding of the K/Ar system, an appreciation of the subtleties of geological material and a continuous refinement of the analytical tools used for isotope extraction and counting. The 40 Ar/ 39 Ar method is also one of the most versatile techniques with countless applications in archaeology, tectonics, structural geology, orogenic processes and provenance studies, ore and petroleum genesis, volcanology, weathering processes and climate, and planetary geology. This volume is the first of its kind and covers methodological developments, modelling, data handling, and direct applications of the 40 Ar/ 39 Ar technique.
Identifying effective interpretation methods for magnetic data by profiling and analyzing human data interactions
36 Cl exposure dating of paleoearthquakes in the Eastern Mediterranean: First results from the western Anatolian Extensional Province, Manisa fault zone, Turkey
Porosity prediction using the group method of data handling
Crustal structure from gravity signatures in the Iberian Peninsula
Estimating surface roughness of terrestrial laser scan data using orthogonal distance regression
Earthquake-cycle deformation and fault slip rates in northern Tibet
Assessment of Mineral Potential Using Cross-Validation Techniques and Statistical Analysis: A Case Study from the Paleoproterozoic of West Greenland
Gold prospectivity maps of the Red Lake greenstone belt: application of GIS technology,
Slip analysis of the Kokoxili earthquake using terrain-change detection and regional earthquake data
Empirical observations from fluvial systems across the globe reveal a consistent power-law scaling between channel slope and contributing drainage area. Theoretical arguments for both detachment- and transport-limited erosion regimes suggest that rock uplift rate should exert first-order control on this scaling. Here we describe in detail a method for exploiting this relationship, in which topographic indices of longitudinal profile shape and character are derived from digital topographic data. The stream profile data can then be used to delineate breaks in scaling that may be associated with tectonic boundaries. The description of the method is followed by three case studies from varied tectonic settings. The case studies illustrate the power of stream profile analysis in delineating spatial patterns of, and in some cases, temporal changes in, rock uplift rate. Owing to an incomplete understanding of river response to rock uplift, the method remains primarily a qualitative tool for neotectonic investigations; we conclude with a discussion of research needs that must be met before we can extract quantitative information about tectonics directly from topography.