All Stories

  1. Impact of salt and frost weathering on the physical and durability properties of travertines and carbonate tufas used as building material
  2. Stone weathering under Mediterranean semiarid climate in the fortress of Nueva Tabarca island (Spain)
  3. Mineralogical evolution of salt over nine years, after removal of efflorescence and saline crusts from Elche’s Old Bridge (Spain)
  4. Predicting water permeability in sedimentary rocks from capillary imbibition and pore structure
  5. A comparison of experimental methods for measuring water permeability of porous building rocks
  6. Microbial dolomite in fresh water carbonate deposits
  7. Non-linear decay of building stones during freeze–thaw weathering processes
  8. Sedimentary structures and physical properties of travertine and carbonate tufa building stone
  9. Comparison of the static and dynamic elastic modulus in carbonate rocks
  10. Mechanical Analysis of Multi-Textural Rocks (Brecciated Dolostones and Limestones): A New Micro-Compression Test for Rocks
  11. Bacterial diversity in dry modern freshwater stromatolites from Ruidera Pools Natural Park, Spain
  12. Bioinduced precipitation of barite and celestite in dolomite microbialites
  13. Rock fabric, pore geometry and mineralogy effects on water transport in fractured dolostones
  14. Deteriorating effects of lichen and microbial colonization of carbonate building rocks in the Romanesque churches of Segovia (Spain)
  15. Recent seismogenic fault activity in a Late Quaternary closed-lake graben basin (Albacete, SE Spain)
  16. Multivariate statistical techniques for evaluating the effects of brecciated rock fabric on ultrasonic wave propagation
  17. Dolomite-silica stromatolites in Miocene lacustrine deposits from the Duero Basin, Spain: the role of organotemplates in the precipitation of dolomite
  18. Salt weathering in dual-porosity building dolostones
  19. Petrographic quantification of brecciated rocks by image analysis. Application to the interpretation of elastic wave velocities
  20. Interaction between Calcite and Phosphorus in Biomineralization Processes in Tufa Carbonates
  21. Temperate and semi-arid tufas in the Pleistocene to Recent fluvial barrage system in the Mediterranean area: The Ruidera Lakes Natural Park (Central Spain)
  22. Role of pore structure in salt crystallisation in unsaturated porous stone
  23. Influence of surface roughness on color changes in building stones
  24. Salt influence on evaporation from porous building rocks
  25. Sedimentology of Quaternary perched springline and paludal tufas: criteria for recognition, with examples from Guadalajara Province, Spain
  26. The water balance equations in saline playa lakes: comparison between experimental and recent data from Quero Playa Lake (central Spain)
  27. Petrographic and geochemical evidence for the formation of primary, bacterially induced lacustrine dolomite: La Roda 'white earth' (Pliocene, central Spain)
  28. Quantification of salt weathering in porous stones using an experimental continuous partial immersion method
  29. Thermodynamic modelling of changes induced by salt pressure crystallisation in porous media of stone
  30. Penecontemporaneous diagenesis in continental saline sediments: bloeditization in Quero playa lake (La Mancha, Central Spain)
  31. Pore size distribution and the durability of a porous limestone
  32. Unusual twinning features in large primary gypsum crystals formed in salt lake conditions, Middle Miocene, Madrid Basin, Spain: palaeoenvironmental implications—reply
  33. Unusual twinning features in large primary gypsum crystals formed in salt lake conditions, Middle Miocene, Madrid Basin, Spain—palaeoenvironmental implications
  34. The physicochemical weathering of monumental dolostones, granites and limestones; dimension stones of the Cathedral of Toledo (Spain)
  35. Palustrine sedimentation and associated features—grainification and pseudo-microkarst—in the Middle Miocene (intermediate unit) of the Madrid Basin, Spain
  36. Endolithic cyanobacteria in Maastricht limestone