The relationship between magnetic anisotropy, rock-strength anisotropy and vein emplacement in gold-bearing metabasalts of Gadag (South India)

0506909 - ÚGN 2020 RIV NL eng J - Journal Article
Vishnu, C. S. - Lahiri, S. - Mamtani, M. A.
The relationship between magnetic anisotropy, rock-strength anisotropy and vein emplacement in gold-bearing metabasalts of Gadag (South India).
Tectonophysics. Roč. 722, January 2018 (2018), s. 286-298. ISSN 0040-1951. E-ISSN 1879-3266
Institutional support: RVO:68145535
Keywords : anisotropy of magnetic susceptibility * metabasalts * rock strength anisotropy * vein emplacement * mineralization
OECD category: Mechanical engineering
Impact factor: 2.764, year: 2018
Method of publishing: Limited access
https://www.sciencedirect.com/science/article/pii/S0040195117303797?via%3Dihub

In this study the importance of rock strength and its anisotropy in controlling vein emplacement is evaluated by integrating anisotropy of magnetic susceptibility (AMS) with rock mechanics data from massive (visibly isotropic) metabasalts of Gadag region (Dharwar Craton, South India). Orientation of magnetic foliation (MF) is first recognized from AMS. Subsequently, rock mechanics tests viz. ultrasonic P-wave velocity (V-p), uniaxial compressive strength (UCS) and point load strength (I-s(50)) are done in cores extracted parallel and perpendicular to MF. V-p is found to be higher in direction parallel to MF than perpendicular to it. In contrast rock strength (UCS and I-s(50)) is greater in direction perpendicular to MF, than parallel to it. This proves that rocks from the gold mineralized belt of Gadag have rock strength anisotropy. Orientation of MF in Gadag region is NW-SE, which is also the mean orientation of quartz veins. Previous studies indicate that emplacement of veins in the region took place during regional D3 (NW-SE shortening). Based on the present study, it is concluded that vein emplacement took place in NW-SE orientation because the rocks have strength anisotropy and are weaker in this direction (orientation of MF), which dilated to accommodate fluid flow. In addition, vein intensities are measured along three traverses and found to be variable. It is argued that since mineralization is favoured when the system gets saturated with fluid, variation in fluid flow could not have been responsible for variation in vein intensities in the study area. Since the rock strength of the different blocks investigated here is not uniform, it is envisaged that variation in rock strength played an important role in controlling the vein intensities. It is concluded that rock strength variation controlled strain partitioning and channelized fluid flow thus influencing vein emplacement and mineralization and formation of lodes.
Permanent Link: http://hdl.handle.net/11104/0298047