Distribution ofMysticellus frankigen. et sp. nov. and its closest generic relativeMicryletta. Map prepared using QGIS 2.6.1 (http://www.qgis.org). Image credits:Micryletta inornata(M.A.M.M. Akil),Micryletta erythropoda(J. Rowley) andMicryletta steinegeri(N.A. Poyarkov Jr.). Full...
Eastwards below the Wynad plateau, however, the shear zone becomes less prominent suggesting local variations in its geometry. The models also point out the presence of a thick high-density body (2.98 g/cc) in the lower part of the crust below the northern charnockite province, which ...
Map scale in kilometers. Source: Elevation data: Global Digital Elevation Model (DEM) from ASTER Full size image Peninsular seaway breaks may explain how the mtDNA discontinuities arose, but a fundamental question remains unanswered: what mechanisms maintain mitochondrial lineages geographically restricted...
Fig. 6. Map of Italy showing the 19 lithological classes identified with both the short ID and the extended name (Bucci et al., 2022). Up to now, there are no studies regarding the provenance of the clay of Italian briquetage vessels. Such studies have exclusively been performed on domest...
Peninsula, was distributed with the 27thRegiment and two mountain batteries in the northern zone, which included Anzac Cove, and the 26thRegiment with one mountain battery in the southern zone, which included Cape Helles. The 25thRegiment, on the Kilid Bahr plateau, formed th...
A significant area under salt affected soils (69%) was found in ACR XI (East Coast Plains and Hills Region), distributed in Tamil Nadu (34%), Andhra Pradesh (19%) and Orissa (15%); followed by 26% in ACR X (Southern Plateau and Hills Region), located in Karnataka (16%), Andhra ...
The Bouguer anomaly map shows the high and lows coinciding with the charnockitic rocks on east and west and the shear zones on north and south of the Nilgiri plateau. The grav- ity derived crustal model indicates a thick crust (44 km) followed by a body of high density 2.98 g/cm3 in...
The steepness of the Moyar and Bhavani shears on either side of Nilgiri plateau indicates uplift of the plateau due to block faulting with a high density mass at the crustal base. The Bhavani Shear Zone is manifested as a steep southerly dipping plane extending to deeper levels along which ...