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Inventarisasi Dan Eksplorasi Mineral Logam Di Daerah Kabupaten Cianjur Dan Kabupaten Sukabumi Provinsi Jawa Barat (Dim-Kigam Fase Iii), Ta

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Inventarisasi Dan Eksplorasi Mineral Logam Di Daerah Kabupaten Cianjur Dan Kabupaten Sukabumi Provinsi Jawa Barat (Dim-Kigam Fase Iii), Ta INVENTARISASI DAN EKSPLORASI MINERAL LOGAM DI DAERAH KABUPATEN CIANJUR DAN KABUPATEN SUKABUMI PROVINSI JAWA BARAT (DIM-KIGAM FASE III), TA. 2004 Oleh : Sahat Simanjuntak, Armin Tampubolon, Kisman, Selo H.J. Sihombing SUBDIT MINERAL LOGAM ABSTRACT The investigation report is resulted from the third phase of joint exploration program between Directorate of Mineral Resources Inventory and Korea Institute of Geoscience and Mineral Resources (KIGAM) taking place within the Southern Mountains of West Java Region. There are two methods that have been performed during this third phase investigation including diamond drilling and general survey. The former took place around Mt.Cilangkap, southern part of Mt. Subang, Tanggeung District, Cianjur Regency. While the latter took place within the mining concession area belonging to Directorate General of Geology and Mineral Resources (WPP DJGSM). Before conducting drilling activity, a grid system of soil geochemistry and systimatical sampling from trenches around Celak quartz vein and Cigadobras quartz vein areas have been done. The results obtained from these activities are the geochemical anomalies for Cu, Pb, Zn, Ag and Au in soil and the interval values of gold contents ranging from 7.8 – 91.1 ppm in the trenches. Diamond drilling in aimed to check subsurface geology in Mt. Cilangkap area was focussed on four bore holes with a total depth of 310 m where the type of drilling machine used during this activity is Koken OE-8. Nothing mineralisation zone has been accountered during this drilling activity. Based on core description, three lithological units have been found, consisting of andesitic lava, lapilli tuff and andesitic breccia.Propyllitic alteration is dominantly observed in most of samples taken from drilling holes although some barren quartz veinlets can be found in core samples. There are 70 samples taken during drilling activities. All of these samples have been analysed for Au, indicating that the highest gold value is up to 0.142 ppm. No gold mineralisation zone has been accountered. This is probably as result of normal faulting system occurred in this region. In this case, Mt. Cilangkap area is inferred as foot wall of the system so that the mineralisation is probably in too deep position and thus may has not been reached by the drilling depth target. The general survey conducted in WPP DJGSM area has not found an indication for metallic deposit in terms of alteration or significant values of metallic elements. The chemical analysis results of rock samples for Au range from 15 ppb to 65 ppb, while for stream sediment samples show a maximum value of 186 ppb Au . Tanggeung, Kabupaten Cianjur, Provinsi Jawa 1. PENDAHULUAN Barat dan penyelidikan regional di dalam Kerjasama eksplorasi mineral logam di WPP yang belum selesai pada tahun Peg. Selatan Jawa Barat dalam WPP DJGSM sebelumnya. antara Direktorat Inventarisasi Sumber Daya Mineral (DIM) - Korea Institute of Geosince 2. HASIL PENYELIDIKAN and Mineral Resources (KIGAM) yang TERDAHULU berlangsung selama tiga tahun (2002-2004) Temuan hasil inventarisasi dan eksplorasi dibagi dalam tiga fase penyelidikan yang dilaksanakan pada fase kedua (TA.2003, (Gambar.1).Fase penyelidikan pendahuluan Simanjuntak Sahat dkk) berupa penyelidikan dilaksanakan pada T.A 2002 Fase kedua geokimia tanah dengan sistim kisi (Grid soil (TA.2003) merupakan fase lanjutan, bertujuan sampling) disekitar urat kuarsa Celak dan untuk meneliti lebih rinci hasil penemuan Cigadobras menemukan sejumlah anomali mineralisasi pada fase pertama serta unsur Cu, Pb, Zn,Ag dan Au serta hasil dari melanjutkan penyelidikan regional dalam tiga parit uji di daerah Gn Cilangkap yang WPP DJGSM. Fase ketiga berupa kegiatan menunjukan kadar unsur logam terutama Au pemboran uji geologi di daerah Gn. Cilangkap 7.8- 91.1 ppm. Diduga mineralisasi logam di (bagian Selatan Gn. Subang) Kecamatan daerah ini diduga terbentuk di dalam batuan Kolokium Hasil Lapangan – DIM, 2005 13-1 gunungapi Miosen Akhir, berupa urat kuarsa arah jurus dan kemiringan urat kuarsa dengan berlapis, berongga dan cockade. arah jurus/kemiringan U320°/70°. Urat kuarsa tersebut memperlihatkan sifat-sifat fisik antara 3. HASIL PENYELIDIKAN FASE III lain massif, keras dan kompak, berwarna putih 3.1. Penyelidikan Rinci Pemboran Uji susu (milky quartz), tampak adanya residual Geologi di Daerah Gn. Cilangkap vuggy silica dan kalsedon. Mineral logam Kecamatan Tanggeung Kab.Cianjur yang teramati diantaranya pirit halus tersebar, kalkopiorit, oksida tembaga, oksida mangan 3.1.1. Geologi Daerah Penyelidikan dan oksida besi. Litologi daerah pemboran uji geologi 3.1.3. Hasil Pemboran Uji didominasi oleh batuan vulkanik terdiri dari batuan tufa lapili dan breksi vulkanik (Gambar Penyelidikan yang dilakukan pada tahun 2). Satuan batuan tufa menempati 2/3 daerah 2003 berupa pembuatan 3 (tiga) parit uji di penyelidikan. Singkapan batuan yang cukup daerah Gn. Cilangkap ini menunjukan kisaran baik hanya ditemukan di sungai Cibuni yang kadar Au 7.8 – 91.1 ppm, sementara hasil terletak di bagian utara lokasi pemboran. analisis kimia unsur yang diambil dari Batuan breksi tersingkap baik disepanjang singkapan batuan tufa terkersikan sungai Cilangkap hingga pada tebing diatas mengandung urat-urat kuarssa halus di puncak sungai atau pada lereng bagian bawah. Satuan Gn. Cilangkap menunjukan kadar Au 0.2 batuan ini dicirikan oleh warna abu-abu ppm...Posisi titik bor, azimuth, inklinasi dan kehijauan.Tampak mineral hitam telah kedalaman lubang bor di daerah ini adalah berubah menjadi klorit dan epidot, disertai seperti pada Tabel 1. kandungan pirit halus tersebar, 1 sampai 3% Tabel 1.Rincian Lokasi Pemboran Uji dengan intensitas lemah sampai kuat Secara Geologi di daerah Gn.Cilangkap, Kec. umum baik singkapan maupun bongkah Tanggeung, Kab. Cianjur. batuan telah mengalami ubahan hidrotermal, No. Koordinat Azimuth Inklinasi Kedala- sehingga batas kedua satuan batuan tersebut Bor man (m) agak sulit dibedakan. Struktur geologi yang CK.1 732236 mE U90° 70° 60 9196889 mN berkembang di daerah ini adalah sesar geser, CK.2 732234 mE U90° 70° 100 berarah tenggara-barat laut dan barat daya- 9197035 mN CK.3 732233 mE U330° 70° 80 timur laut, serta sesar normal berarah timur- 9197164 mN barat dan tenggara-barat laut. CK.3 732236 mE U330° 70° 70 9196893 mN 3.1.2. Ubahan dan Mineralisasi Sebanyak 70 conto batuan hasil dari inti Mineralisasi Gn. Cilangkap terletak di bor telah diambil dan dianalisis untuk lembah Sungai Cilangkap (Cabang Sungai mengetahui kadar logamnya (Cu,Pb,Zn,Ag Cibuni) yang dipisahkan oleh sungai Cibuni dan Au). Hasil pengamatan inti bor dari pada ketinggian 200 –500 m diatas permukaan keempat lubang bor tersebut dapat dijelaskan laut. Ubahan batuan yang berkembang pada tabel 2 ,3, 4 dan 5 serta gambar 3 dan 4. didaerah ini terdiri dari 3 (tiga) jenis yaitu : (a) Propilitisasi dicirikan oleh hadirnya Tabel 2. Hasil pemerian lubang bor CK.1 mineral klorit + epidot + karbonat + serisit. Kedalaman Pemerian (b) Argilitisasi, dicirikan oleh hadirnya ( m) mineral kaolinit + illite + serisit/paragonit (c) 0.00-5.00 : Soil,coklat kekuningan bercampur dengan Silisifikasi dicirikan oleh penambahan mineral fragmen batuan berbutir halus. silica (SiO2) umumnya ditemukan pada zona 5.00-17..90 : Lava andesit, abu-abu kehijauan, halus, urat atau pada zona mineralisasi terutama terpropilitkan lemah, urat-urat kalsit pada perbukitan terjal. Para penambang lokal 1mm-3 cm, minor pirit telah melakukan penambangan dengan cara 17.90-60.00 : Breksi Andesit, abu-abu kehijauan, membuat lubang bukaan/adit yang pada terpropilitkan lemah-sedang, urat-urat umumnya berarah ke utara-selatan.. kalsit, minor pirit. Sedikitnya ada 6 adit yang dijumpai, tetapi Analisis kimia unsur sebanyak 8 conto hanya 3 adit yang dimasuki, karena sebagian menunjukan kisaran kadar Cu : 21-107 ppm, adit tertutup vegetasi yang rimbun dan Pb: 15 – 26 ppm, Zn: 51-88 ppm Ag 1- 3 ppm longsor. Berdasarkan pengamatan, dan Au : 0.004 – 0.017 ppm. mineralisasi dalam satu adit berukuran lebar 1m, tinggi 1.5 m dengan arah 320° diperoleh Kolokium Hasil Lapangan – DIM, 2005 13-2 Tabel 3. Hasil pemerian lubang bor CK.2 Dari hasil analisis kimia unsur sebanyak 25 conto menunjukan kisaran kadar Cu : 15- Kedalaman Pemerian ( m) 235 ppm, Pb: 14 – 266 ppm, Zn: 69-349 ppm, Ag 1- 68 ppm dan Au : 0.005 – 0.124 ppm. 0.00-6.50 : Soil,coklat kekuningan bercampur dengan fragmen batuan berbutir kasar Hasil analisis kimia unsur sebanyak 16 6.50-14.16 : Tufa, halus, kuning kecoklatan-abu-abu conto menunjukan kisaran kadar Cu : 7-122 kehijauan, bagian atas lapuk(6.50-9.00 m), bagian tengah hingga bagian bawah ppm, Pb: 11 – 28 ppm, Zn: 63-276 ppm, Ag 1- terkloritkan lemah sampai sedang, pada 3 ppm dan Au : 0.0013 – 0.042 ppm. beberapa tempat terkaolinkan lemah (19.35 m) 2. Penyelidikan Regional di daerah 14.16-53.38 : Tufa lapili, abu-abu putih – abu-abu Kecamatan Ciracap Kabupaten Sukabumi. kehijauan, porous, beberapa retak-retak, bagian tengah hingga bagian bawah Berdasarkan pengamatan lapangan terpropilitkan lemah sampai sedang, urat kalsit berbagai arah, limonit staining stratigrafi daerah ini mulai dari batuan tua mengisi retakan, minor pirit). hingga batuan muda adalah sebagai berikut (Gambar 5) : 14.16-53.38 : Tufa lapili, abu-abu putih – abu-abu kehijauan, porous, beberapa retak-retak, bagian tengah hingga bagian bawah 1. Satuan batuan lava andesit-basaltik, terpropilitkan lemah sampai sedang, urat terdapat dibagian baratlaurt daerah kalsit berbagai arah, limonit staining mengisi retakan, minor pirit).
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