Incomplete Solution: Weathering of Cave Walls and the Production, Transport and Deposition of Carbonate Fines
Coronet Books Incorporated, 2003 - 167 strani
"The studies reported in this book investigated the little explored subject of incomplete solution of limestones and dolomites. There was a surprising presence of significant quantities of carbonate clasts in cave sediments as well as an occurrence of thick, soft zones of an unknown mineral on the walls of cave passages. Contents include: Weathering of Limestone and Dolomite in the Cave Environment, Formation of Autochthonous Carbonate Clasts, and Conclusions."
Mnenja - Napišite recenzijo
Na običajnih mestih nismo našli nobenih recenzij.
amount analyses becomes bedding plane bottom brezno calcite calcite veins carbonate rock carried cave passages cave walls ceiling channels chemical clastic clastic sediments clay minerals colour completely concentration consists contains corrosion covered cross-section crust crystal deposits depth developed direction discoloured dissolution dissolved dolomite edge entirely entrance ered erosion Figure fissures flow flowstone formation fresh Geological grains grey increased indicates insoluble residue ions jama kamnine karst layer less light limestone and dolomite Ljubljana lower measured mechanical method micrite Mihevc mineral composition moisture occur origin particles passage walls Pečina v Borštu places points pores porosity porous precipitation present Prevali processes quantities quartz ratio remains sample sand sediments selective shafts silt solution surface texture thick thin tion traces transport upper voda washed weath weathered limestone weathered rock weathered wall weathered zone