Chondrites isp. Indicating Late Paleozoic Atmospheric Anoxia in Eastern Peninsular India
Figure 2
Generalized sedimentary logs of the Barakar Formation in (a) Raniganj Basin and (b) Talchir Basin. The study sections are marked and are detailed in Figure 3(a) (Khudia Nala) nad Figure 3(b) (Kudaposi Nala), respectively.
