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1. How Do Secondary Minerals in Granite Help Distinguish Paleo- from Present-Day Permeable Fracture Zones? Joint Interpretation of SWIR Spectroscopy and Geophysical Logs in the Geothermal Wells of Northern Alsace

2. How Do Secondary Minerals in Granite Help Distinguish Paleo- from Present-Day Permeable Fracture Zones? Joint Interpretation of SWIR Spectroscopy and Geophysical Logs in the Geothermal Wells of Northern Alsace

3. Clay Minerals in the Deep Reservoir of the Cerro Pabellón Geothermal System (Northern Chile)

4. Clay Mineralogy: A Signature of Granitic Geothermal Reservoirs of the Central Upper Rhine Graben

6. Quantitative evolution of the petrophysical properties of andesites affected by argillic alteration in the hydrothermal system of Petite Anse-Diamant, Martinique

7. Experimental formation of clay-coated sand grains using diatom biofilm exopolymers

8. Significance of the depth-related transition montmorillonite-beidellite in the Bouillante geothermal field (Guadeloupe, Lesser Antilles)

9. Mapping 238U decay chain equilibrium state in thin sections of geo-materials by digital autoradiography and microprobe analysis

10. Formation of stromatolite lamina at the interface of oxygenic–anoxygenic photosynthesis

11. Contribution of the Paragenetic Sequence of Clay Minerals to Re-Examination of the Alteration Zoning in the Krafla Geothermal System

12. The record of environmental and microbial signatures in ancient microbialites : the terminal carbonate complex form the Neogene basins of southeastern Spain

13. Influence of sedimentation and detrital clay grain coats on chloritized sandstone reservoir qualities: Insights from comparisons between ancient tidal heterolithic sandstones and a modern estuarine system

14. Alteration halos in the Tordillos sediment-hosted copper deposit of the Neuquén Basin, Argentina

15. Facies associations, detrital clay grain coats and mineralogical characterization of the Gironde estuary tidal bars: A modern analogue for deeply buried estuarine sandstone reservoirs

16. How do the geological and geophysical signatures of permeable fractures in granitic basement evolve after long periods of natural circulation? Insights from the Rittershoffen geothermal wells (France)

17. Mineral reactions associated with hydrocarbon paleomigration in the Huincul High, Neuquén Basin, Argentina

18. Mineralogical signature of hydrocarbon circulation in Cretaceous red beds of the Barda Gonzalez area, Neuquen Basin, Argentina

19. Chlorite, white mica and clay minerals as proximity indicators to ore in the shallow porphyry environment of Quebrada de la Mina deposit, Argentina

20. Microbial and diagenetic steps leading to the mineralisation of Great Salt Lake microbialites

21. Clay minerals related to circulation of near neutral to weakly acidic fluids in active high energy geothermal systems

22. Spatial and temporal evolution of hydrothermal alteration at Lavras do Sul, Brazil: evidence from dioctahedral clay minerals

23. Significance of the depth-related transition montmorillonite-beidellite in the Bouillante geothermal field (Guadeloupe, Lesser Antilles)

24. Significance of aluminum phosphate-sulfate minerals associated with U unconformity-type deposits: The Athabasca basin, Canada

25. Mineralogy and geochemistry of the host-rock alterations associated with the Shea Creek unconformity-type uranium deposits (Athabasca Basin, Saskatchewan, Canada). Part 1. Spatial variation of illite properties

27. Occurrence of K-feldspar bearing hydrothermal breccias in the Bouillante geothermal field (Basse Terre - Guadeloupe)

28. Application of chemical geothermometry to low-temperature trioctahedral chlorites

29. Clay minerals in basalt-hawaiite rocks from Mururoa Atoll (French Polynesia). II. petrography and geochemistry

30. Clay minerals in basalt-hawaiite rocks from mururoa atoll (French polynesia). I. mineralogy

31. Mineralogy and geochemistry of the host-rock alterations associated with the shea creek unconformity-type uranium deposits (Athabasca Basin, Saskatchewan, Canada). Part 2. Regional-scale spatial distribution of the Athabasca group sandstone matrix minerals

32. A cloritização na Mina Uruguai, Minas do Camaquã, RS, Brasil

33. Crystal size of epidotes: A potentially exploitable geothermometer in geothermal fields?

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