Occurrence and mineralogical characterization of specularite in Damjan ore deposit, North Macedonia

In this paper are presented occurrence and mineralogical characterization of specularite from Damjan ore deposit. The straightforward identification of the studied mineral sample was enabled by SEM-EDS, XRF and XRPD methods. With these methods it can be seen that the phases present are calcite, specularite and quartz. Specularite crystals occur in the surface parts of the deposit. Specularite has a metallic gray to silvery appearance with a glittering luster and reddish streak. It shows a very smooth surface with reflection. The metallic luster is a result of the specific crystal formation of hematite. Manganese and aluminium substitute for Fe³⁺ in the specularite structure. Small amounts of Fe²⁺ and Mn2+ substitute for Ca²⁺ in the crystal lattice on calcite. The well-developed morphology of specularite suggests that it crystallized first. The finer-grained calcite likely formed later, filling the interstitial spaces between the earlier-formed specularite. Key words: specularite; calcite; quartz; Damjan

Authors

Publication Details

Journal
Goce Delchev University Repository (Goce Delčev University of Štip)
Published
2025-12-01
Primary Topic
Clay minerals and soil interactions
Type
article
Field-Weighted Citation Impact
0.00
Controls
|||
ALL TIME
JAN
FEB
MAR
APR
MAY
JUN
JUL
AUG
SEP
OCT
article

Occurrence and mineralogical characterization of specularite in Damjan ore deposit, North Macedonia

Ivan Boev, Lidija Robeva-Čukovska, Tena Šijakova-Ivanova
Goce Delchev University Repository (Goce Delčev University of Štip)
Clay minerals and soil interactions
article

Occurrence and mineralogical characterization of specularite in Damjan ore deposit, North Macedonia

Ivan Boev, Lidija Robeva-Čukovska, Tena Šijakova-Ivanova
article en

Abstract

In this paper are presented occurrence and mineralogical characterization of specularite from Damjan ore deposit. The straightforward identification of the studied mineral sample was enabled by SEM-EDS, XRF and XRPD methods. With these methods it can be seen that the phases present are calcite, specularite and quartz. Specularite crystals occur in the surface parts of the deposit. Specularite has a metallic gray to silvery appearance with a glittering luster and reddish streak. It shows a very smooth surface with reflection. The metallic luster is a result of the specific crystal formation of hematite. Manganese and aluminium substitute for Fe³⁺ in the specularite structure. Small amounts of Fe²⁺ and Mn2+ substitute for Ca²⁺ in the crystal lattice on calcite. The well-developed morphology of specularite suggests that it crystallized first. The finer-grained calcite likely formed later, filling the interstitial spaces between the earlier-formed specularite. Key words: specularite; calcite; quartz; Damjan

Goce Delchev University Repository (Goce Delčev University of Štip)
Openalex Percentile: Top 43%
Clay minerals and soil interactions
AI Navigator

Ask Laika to Summarize, Analyze, and Connect papers live on the map.

Summarize Papers & Methodologies

Extract key findings, datasets, and comparative methods across publications.

Benchmark Rankings & Visual Analytics

Rank top research institutions, authors, funders, topics, and journals by Field-Weighted Citation Impact (FWCI) and paper volume with instant charts.

Connect Distant Disciplines

Bridge topological clusters on the map to find hidden collaborative intersections.

Occurrence and mineralogical characterization of specularite in Damjan ore deposit, North Macedonia — Ivan Boev, Lidija Robeva-Čukovska, et al. · Goce Delchev University Repository (Goce Delčev University of Štip) (2025) | TGRS Research Map | TGRS