Compositional and textural analysis of host-rock diamictite matrix at the Kakula copper deposit, Democratic Republic of Congo
Date
2019-10-11
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Abstract
The Kakula deposit is a high-grade sedimentary-rock-hosted Cu deposit (628 Mt, 2.72%
Cu indicated resource, 1% cut-off) ~10 km south of the Kamoa deposit (759 Mt, 2.57%
Cu indicated resource, 1% cut-off) in the central African copperbelt, Democratic
Republic of Congo. Copper-sulphide ore (chalcocite, bornite, chalcopyrite) at Kakula is
predominantly disseminated in the fine-grained matrix of clast-poor (≤20% clasts ≥2
mm) subaqueous debrite (diamictite), at the base of the nearly flat-lying midNeoproterozoic “grand conglomérat” (Mwale formation). Scanning electron microscopy
was used to document matrix texture and composition to develop a matrix paragenesis,
recorded in five phases of the matrix evolution: sedimentation, pre-ore diagenesis, mainore mineralisation, post-ore alteration, and weak tectonism. The ore-zone matrix is
porous, up to 12.5%, and consists of clay- to silt-sized muscovite, quartz, chlorite, Kfeldspar, dolomite, and biotite, whereas least-altered matrix, several hundred metres
above copper-sulphide mineralisation, consists of clay- to silt-sized quartz, albite,
chlorite, K-feldspar, calcite, and dolomite. Copper-sulphide precipitation is
contemporaneous with chlorite and biotite (+/- hematite, quartz, and K-feldspar) and fit in
a paragenetic sequence between diagenetic pyrite (± Fe-dolomite) and later muscovite.
Hematite is ore-stage and most abundant in areas containing chalcocite. Areas of mm- to
cm-scale “aligned” matrix (nearly vertical microfabric of aligned, elongated grains)
consists of a higher abundance of muscovite, locally elongated copper-sulphides, and a
lower concentration of copper than non-aligned matrix, suggesting that copper-sulphide
development pre-dated fabric development and that copper-sulphide grains were later dissolved and possibly remobilised. Although determining the original mineralogy and
texture of the diamictite matrix is challenging, the depositional matrix characteristics
(clast-rich versus clast-poor diamictite) and the availability of reactive agents (e.g.,
diagenetic pyrite) may have been important controls on copper grade and distribution.
More work is required to constrain the absolute timing of mineralisation, which is a
major debate at Kakula and Kamoa.
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Keywords
Kakula deposit, Kamoa deposit, Democratic Republic of Congo, Copper-sulphide ore, matrix paragenesis, central African copperbelt (CACB), fine-grained disseminations, host-rock diamictite matrix