Open Access Open Access  Restricted Access Subscription Access
Open Access Open Access Open Access  Restricted Access Restricted Access Subscription Access

Trace Fossils from the Ordo-Silurian Rocks of Kinnaur, Himachal Himalaya


Affiliations
1 529, Sector 18B, Chandigarh 160018, India
     

   Subscribe/Renew Journal


Ichnofossils Teichichnus, Phycodes aff. palmatum, Planolites, Ichnogenus indet. A and B, and Phycodes circinatum, P. aff. palmatum, Skolithos, Rouaultia and Planolites are being reported respectively from the basal and middle parts of the Yamrang La Formation of Ordovician age. Arthrophycus, Chondrites, Planolites, Rusophycus, Skolithos and Ichnogenus indet, C occur in the basal part of the Manchap Formation of silurian age. Phycodes circinatum Magdefrau 1934 mainly know from Lower Ordovician probably represents an Upper Ordovician age in this area.
Subscription Login to verify subscription
User
Notifications
Font Size

Abstract Views: 208

PDF Views: 4




  • Trace Fossils from the Ordo-Silurian Rocks of Kinnaur, Himachal Himalaya

Abstract Views: 208  |  PDF Views: 4

Authors

O. N. Bhargava
529, Sector 18B, Chandigarh 160018, India
U. K. Bassi
529, Sector 18B, Chandigarh 160018, India
Suresh Chopra
529, Sector 18B, Chandigarh 160018, India

Abstract


Ichnofossils Teichichnus, Phycodes aff. palmatum, Planolites, Ichnogenus indet. A and B, and Phycodes circinatum, P. aff. palmatum, Skolithos, Rouaultia and Planolites are being reported respectively from the basal and middle parts of the Yamrang La Formation of Ordovician age. Arthrophycus, Chondrites, Planolites, Rusophycus, Skolithos and Ichnogenus indet, C occur in the basal part of the Manchap Formation of silurian age. Phycodes circinatum Magdefrau 1934 mainly know from Lower Ordovician probably represents an Upper Ordovician age in this area.