MINERAGRAFI BATUAN PENYUSUN TAMBANG DEEP MILL LEVEL ZONE (DMLZ) PT. FREEPORT INDONESIA

. Ruswanto, Mega Fatimah Rosana, Euis Tintin Yuningsih, Bambang Antoro Purwaiswanto

Abstrak


ABSTRAK

Deep Mill Level Zone (DMLZ) merupakan bagian dari cebakan East Erstberg Skarn System (EESS) dan merupakan tambang bawah tanah level ke-empat setelah Tambang Gunung Bijih Timur (GBT), Intermediate Ore Zone (IOZ) dan Deep Ore Zone (DOZ), yang memiliki cadangan sebesar 472 juta ton, dengan kadar tembaga 0,85% dan emas 0,72 g/t. Mineral bijih yang ditemukan berdasarkan analisa mineragrafi di DMLZ adalah kalkopirit, bornit, kovelit, hematit, sfalerit, galena dan pirit. mineral kalkopirit saling terikat dengan mineral pirit, galena dan sfalerit di batuan intrusi, kalkopirit berikatan dengan sfalerit di batugamping Ekmai, kalkopirit terlihat sebagai butiran bebas dan juga berikatan dengan pirit di batuserpih Ekmai, serta kalkopirit-sfalerit-bornit saling berikatan dan kalkopirit terlihat sebagai inklusi di dalam sfalerit dan juga kovelit hadir menggantikan bornit di beberapa bagian

 

Kata kunci: Deep Mill Level Zone (DMLZ), East Ertberg Skarn System (EESS), mineragrafi, mineral bijih.

 

ABSTRACT

Deep Mill Level Zone (DMLZ) is one of underground mining in PT. Freeport Indonesia and part of East Erstberg Skarn System (EESS) Complex, located at 4th level below Gunung Bijih Timur (GBT), Intermediate Ore Zone (IOZ) dan Deep Ore Zone (DOZ) with reserve 472 milion ton with garde of Cu 0.85% and Au 0.72 g/t. Ore minerals in DMLZ based on minergraphy are chalcopyrite, bornite, covelite, hematit, sphalerite, galena and pyrite. Chalcopyrite minerals binds with pyrite-galena-sphalerite in intrusive rocks, chalcopyrite binds to sphalerite in the Ekmai limestone, chalcopyrite is seen as free-grained and binds to pyrite in the Ekmai shalestone, as well as chalcopyrite-sphalerite binding and viscous chalcopyrite as inclusions in the sphalerite and present covelite to replace the bornite in some parts

 

Key words: Deep Mill Level Zone (DMLZ), East Ertberg Skarn System (EESS), mineragraphy, Ore minerals.


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Referensi


DAFTAR PUSTAKA

Gandler, L.M., and Kyle, J.R., 2008, Stratigraphic Control of Calc-Silicate Alteration and Cu-Au Mineralization of the Deep MLZ Skarn, Ertsberg District, Papua, Indonesia. PACRIM Conference, 2008.

PT. Freeport Indonesia, 2015, Revisi Feasibility Study Bab 3. Geologi dan Geologi Teknik, tidak diterbitkan.

Quarles van Ufford, A. I, and Closs, M, 2005, Cenozoic Tectonics of New Guinea, AAPG Bulletin, vol. 89, No. 01, p. 119-140

Quarles van Ufford, A. I, and Closs, M, 2005, Cenozoic Tectonics of New Guinea, AAPG Bulletin, vol. 89, No. 01, p. 119-140.

Sapiie, B., 2016, Kinematic Analysis of Fault-Slip Data in the Central Range of Papua, Indonesia. Indonesian Journal on Geoscience Vol.3 No.1 April 2016, pages 1-6.

Sunyoto, W., De Jong, G., dan Soebari, L., 2012, Porphyry and Skarn Cu-Au Deposits and its Associated Cu-Au Bearing Intrusions of the Ertsberg District, Papua, Indonesia. Proceeding Of Banda And Eastern Sunda Arcs 2012, MGEI Annual Convention. 279-281)

Sunyoto, W., MacDonald, G., and De Jong, G., 2015, From Discovery to Inventory – PT. Freeport Indonesia Story in Papua Province, Indonesia. HAGI-IAGI-IAFMI-IATMI Joint Convention, Balikpapan, 2-4 October 2015.




DOI: https://doi.org/10.24198/bsc.v15i2.13836

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