شماره ركورد كنفرانس :
4640
عنوان مقاله :
Geomorphology of Iran Zagros Gulf
عنوان به زبان ديگر :
Geomorphology of Iran Zagros Gulf
پديدآورندگان :
kheyrodin Hamid kheyrodin@semnan.ac.ir Assistant professor semnan university Iran؛Mail:hamid
كليدواژه :
Gulf , geomorphology , earth
عنوان كنفرانس :
ششمين همايش ملي ژئومورفولوژي و چالش هاي پيش رو
چكيده فارسي :
Geomorphology is a science that deals with the relief features of the earth or of another celestial body (such as the moon) and seeks an interpretation of them based on their origins and development.Geomorphology is the study of the characteristics, origin, and development of landforms. The movements of the earth s crust can be divided into two general categories of orogenic and epeirogenic movements. The orogeny movement refers to those crust movements that cause rapid deformation of large masses of rocks with short duration of its impact on a geological scale and high intensity; these movements cause faults, folds and mountains. The epeirogenic movements include movements of the earth s crust whose duration of impact is long and whose severity is low, such as downward movement of crust and formation of basins, as well as rise of parts of the crust. The epeirogenic movements cause the seas’ receding and advancing.
چكيده لاتين :
Geomorphology is a science that deals with the relief features of the earth or of another celestial body (such as the moon) and seeks an interpretation of them based on their origins and development.Geomorphology is the study of the characteristics, origin, and development of landforms. The movements of the earth s crust can be divided into two general categories of orogenic and epeirogenic movements. The orogeny movement refers to those crust movements that cause rapid deformation of large masses of rocks with short duration of its impact on a geological scale and high intensity; these movements cause faults, folds and mountains. The epeirogenic movements include movements of the earth s crust whose duration of impact is long and whose severity is low, such as downward movement of crust and formation of basins, as well as rise of parts of the crust. The epeirogenic movements cause the seas’ receding and advancing.