Abstract
Pedestal mountains of Gobi type, distinguished by N.A. Florensov, are not arched, since there often is intramountain depression in their axial part, dividing the whole ridge into two separate having mutual pedestal. Small ridges - the mountains of the basins bottom, which undergo an initial stage of the Gobi type orogenesis, represent the earliest stage of pedestal mountains formation.
Full Text 
Sign-in/Register to access full text options
Sign-in/Register to access full text options 
Published version (
Free)
Free) 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a call
