Point load strength of granodiorites from the Plana pluton-Reference-Cited by-同舟云学术

Point load strength of granodiorites from the Plana pluton

Published:2018 Issue:1 Volume:32 Page:49-56
ISSN:2738-6996
Container-title:Engineering Geology and Hydrogeology
language:
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Author:

Ivanov Plamen¹^ORCID,Nankin Rosen¹^ORCID,Krastanov Miroslav¹^ORCID

Affiliation:

1. Geological Institute, Bulgarian Academy of Sciences, Acad. G. Bonchev Str., Bl. 24, 1113 Sofia, Bulgaria

Abstract

The studied area is located in the southeast parts of the Plana Mountain. It is built up of Plana diorite pluton, represented by granodiorites, quartz-diorites and quartz-monzonites, which is located among the older (Precambrian) metamorphic rocks (gneisses, amphibolites, schists and fillites). Plana Pluton is part of Tsentralnosrednogorska magmatic province. The aim of the present work is to clarify the physico-mechanical properties of rocks from the Plana pluton in the area of village of Gorni Okol. For this purpose the values of Point load strength index Is(50), water absorption, bulk density, etc. are determined. Correlation dependencies between the studied parameters are revealed.

Publisher

Geological Institute, Bulgarian Academy of Sciences

Reference11 articles.

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