Petrochemical study of Middle-Late Paleozoic sedimentary and
The great meandering of Tuul River is located in the Khentii section of the Khangai-Khentii orogenic belt, Central Mongolia. At the study area, dominanty distributed sedimentary and metamorphic roks of venlok-lower Devonian Sugnugur Formation of Asralt Khairkhan terrane and Pensilvanian Altan-Ovoo Formation of Ulaanbaatar terrane. The …