The fossilized soils in the Paleozoic formations of the kirgiz mountain ridge (North Tien Shan)

摘要

On base of the study of carbonatic concretions, which were exposed on many levels of ortoc suite's section, the conclusion about their belonging to paleo-soil is done. The peculiarities of the concretionary horizon structure letus to select three climatic situations of the soil forming, such as humidity, humidity with signs of an aridness (transiting one) and feebly arid.