Abstract
Some new lithostratigraphic measures are introduced for the nature of existence or removal of some rock units between some studied wadies in Tansulukh area. Lithostratigraphic correlation of the exposed rock units (Middle Eocene-Upper Miocene) between sectors 1-5 in Tansulukh region was necessary to be conducted because of the suspected rock complexities between these sectors. According to the conducted lithostratigraphic correlation between studied sectors (1-5) the missing of OligoceneMiddle Miocene rock units toward sectors 4 & 5 was attributed to some paleo-structural instability during post Eocene till pre-Late Miocene times.
Full Text 
Sign-in/Register to access full text options
Sign-in/Register to access full text options 
Paper version not known
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
