The raw measurement data (the files that come straight from the magnetometer) and raw data with directions from the Upper Permian-Lower Triassic limestones.
The Pachmarhi dyke swarms, situated in the Eastern part of the Narmada-Satpura-Tapi (N-S-T) dykes of the Deccan Continental Flood Basalt (DCFB), are studied using the Anisotropy of Magnetic Susceptibi
Paleomagnetic, rock magnetic, or geomagnetic data found in the MagIC data repository from a paper titled: Anomalous and Reversed Paleomagnetic Field Directions from the Miocene Lovejoy Basalt, Norther
