The Zemo Imereti Plateau is located in the easternmost part of the limestone region of western Georgia and is Caucasus’ only karst plateau. It is centrally located in a relatively elevated part of the intermountain p...The Zemo Imereti Plateau is located in the easternmost part of the limestone region of western Georgia and is Caucasus’ only karst plateau. It is centrally located in a relatively elevated part of the intermountain plain of the country of Georgia. Lithostratigraphical (petrographic, mineralogical, and XRD) research on terrigenous sediments found in caves in the region was conducted in the Upper Cretaceous limestones located at different hypsometric levels (400 - 700 m). This study focused on allochthonous deposits, which, due to sedimentological features, contains significant and complete information for paleogeographic reconstruction as opposed to the autochthonous sediments. Source provinces of the sediments’ origin were determined using petrographic analysis. Lithological study of the terrigenous sediments indicated their origin from the Racha range, as well as their transportation mechanisms, and sedimentation conditions during deposition. Approximate ages (the end of the Middle Pleistocene and the beginning of the Late Pleistocene) of ancient terrestrial sediments in Rganisklde Cave were achieved by taking into account the geological and geomorphological development of the region. Lithostratigraphical analysis of the cave deposits and modern archaeological data indicate that the formation of the caves in the Zemo Imereti plateau took place mainly during the end of the Middle Pleistocene and in the beginning of the Pleistocene;while on the southern slope of the Racha range and in the surrounding area of Ertso-Tsona (Caucasus southern slope), they formed in the Early Pleistocene.展开更多
The history of karst terrestrial development has been restored on the background of many years’ field, experimental and laboratory researches (underground water tracing, structural deciphering of aerophotocytes, anal...The history of karst terrestrial development has been restored on the background of many years’ field, experimental and laboratory researches (underground water tracing, structural deciphering of aerophotocytes, analysis of boreholes and geological wounds) and analysis of the current literary sources carried out by us in the Zemo Imereti Plateau. Within the study area, karst and karst forms of the Jurassic-Cretaceous, Lower Tertiary (Paleocene-Eocene) and Post-Miocene (Sarmati) period were revealed. Lithobiostratigraphic analysis of cave subterranean sediments enabled us to identify the cave age. In Zemo Imereti Plateau, in the caves located on higher hypsometric levels, the sedimentation of subterranean sediments began in the Middle-Upper Pleistocene and it seemed that the caves’ formation was mainly completed in the mentioned territory.展开更多
文摘The Zemo Imereti Plateau is located in the easternmost part of the limestone region of western Georgia and is Caucasus’ only karst plateau. It is centrally located in a relatively elevated part of the intermountain plain of the country of Georgia. Lithostratigraphical (petrographic, mineralogical, and XRD) research on terrigenous sediments found in caves in the region was conducted in the Upper Cretaceous limestones located at different hypsometric levels (400 - 700 m). This study focused on allochthonous deposits, which, due to sedimentological features, contains significant and complete information for paleogeographic reconstruction as opposed to the autochthonous sediments. Source provinces of the sediments’ origin were determined using petrographic analysis. Lithological study of the terrigenous sediments indicated their origin from the Racha range, as well as their transportation mechanisms, and sedimentation conditions during deposition. Approximate ages (the end of the Middle Pleistocene and the beginning of the Late Pleistocene) of ancient terrestrial sediments in Rganisklde Cave were achieved by taking into account the geological and geomorphological development of the region. Lithostratigraphical analysis of the cave deposits and modern archaeological data indicate that the formation of the caves in the Zemo Imereti plateau took place mainly during the end of the Middle Pleistocene and in the beginning of the Pleistocene;while on the southern slope of the Racha range and in the surrounding area of Ertso-Tsona (Caucasus southern slope), they formed in the Early Pleistocene.
文摘The history of karst terrestrial development has been restored on the background of many years’ field, experimental and laboratory researches (underground water tracing, structural deciphering of aerophotocytes, analysis of boreholes and geological wounds) and analysis of the current literary sources carried out by us in the Zemo Imereti Plateau. Within the study area, karst and karst forms of the Jurassic-Cretaceous, Lower Tertiary (Paleocene-Eocene) and Post-Miocene (Sarmati) period were revealed. Lithobiostratigraphic analysis of cave subterranean sediments enabled us to identify the cave age. In Zemo Imereti Plateau, in the caves located on higher hypsometric levels, the sedimentation of subterranean sediments began in the Middle-Upper Pleistocene and it seemed that the caves’ formation was mainly completed in the mentioned territory.
