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Abstrak :
Proses magmatisme berkaitan dengan jalur tektonik ring of fire, yang menyebabkan proses mineralisasi hidrotermal sehingga membentuk potensi sumber daya mineral di Indonesia. Salah satu endapan hidrotermal yaitu endapan epitermal sulfidasi rendah yang berada di Lapangan “RD”, Cibaliung. Struktur patahan menjadi pengontrol sistem epithermal sulfidasi rendah sebagai tempat terendapkannya mineral emas. Integrasi data geologi dengan geofisika diperlukan dalam menentukan struktur pengontrol dan zona potensi mineralisasi. Mineral bijih sulfida dapat dibedakan dari sifat kemagnetan dan kelistrikan dikarenakan mineral logam memiliki respon suseptibilitas, resistivitas dan chargeabilitas lebih tinggi dibandingkan dengan mineral non-logam. Zona potensi mineralisasi emas sulfidasi rendah berada pada zona struktur yang didominasi alterasi argilik dan kaya akan mineral sulfida pada alterasi argilik ilitik dengan nilai suseptibilitas menengah hingga tinggi kisaran -83.7 nT – 92.3 nT, resistivitas dengan nilai rendah hingga menengah 0 – 25 ohm.m dan chargeabilitas dengan nilai menengah hingga tinggi 15 - >75 msec. Dari ketiga parameter tersebut, diduga zona mineralisasi berada pada zona struktur patahan berorientasi Baratlaut-Tenggara. Struktur pengontrol zona potensi mineralisasi tersebut berada di lintasan 3 yaitu patahan D dip 62° ke arah NE dan patahan E dip 83° ke arah NE. Lintasan 4 yaitu patahan D dip 79° ke arah NE, patahan E dip 77° ke arah NE dan patahan F dip 73° ke arah NE. Lintasan 7 yaitu patahan D dip 80° ke arah SW dan patahan E dip 75° ke arah NE. Lintasan 8 yaitu patahan D dip 84° ke arah NE dan patahan E dip 66° ke arah NE. Lintasan 9 yaitu patahan A dip 70° ke arah SW dan patahan B dip 81° ke arah NE. ......The magmatism process is related to the Ring of Fire tectonic pathway, which causes a hydrothermal mineralization process to form potential mineral resources in Indonesia. One of the hydrothermal deposits is an epithermal low-sulfidation deposit in the "RD" Field, Cibaliung. The fault structure controls the epithermal low-sulfidation system as a place for gold mineral deposition. Integration of geological data with geophysical data is required in determining the controlling structure and potential mineralization zone. Sulfide ore minerals can be distinguished from their magnetic and electrical properties because metal minerals have a higher susceptibility, resistivity and chargeability response compared to non-metallic minerals. The potential zone of low sulfidation gold mineralization is located in the structure zone which is dominated by argillic alteration and rich in sulphide minerals in Illitic argillic alteration has medium to high susceptibility values ranging from -83.7 nT - 92.3 nT, resistivity with low to medium values 0 - 25 ohm.m and chargeability with medium to high values of 15 -> 75 msec. From those three parameters, it is assumed that the mineralization zone is located in the NW-SE oriented fault structure zone. The controlling structure for the zone of mineralization potential is in line 3 is fault D with dip 62° to the NE and the E fault with dip 83° to the NE. Line 4 is fault D with dip 79° to the NE, fault E with dip 77° to the NE and fault F with dip 73° to the NE. Line 7, is fault D with dip 80 ° to the SW and the E fault dip 75° to the NE. Line 8 is fault D with dip 84° to the NE and fault E with dip 66 ° to the NE. Line 9 is fault A with dip 70° SW and fault B with dip 81° to NE.

Abstrak :
Lapangan Wabu merupakan daerah prospek mineralisasi emas yang terletak di Kabupaten Intan Jaya, Papua Tengah. Investigasi lebih lanjut perlu dilakukan untuk memperkuat bukti keterdapatan zona prospek mineralisasi emas di wilayah tersebut sebelum dilakukan penambangan. Metode gravitasi dan resistivity-IP dimanfaatkan untuk mengetahui keberadaan struktur geologi dan pola sebaran mineralisasi emas di lapangan Wabu. Pada Penelitian ini data gravitasi GGMplus diolah hingga didapatkan peta anomali residual yang kemudian dilakukan filter FHD dan SVD.  Berdasarkan analisis FHD dan SVD pada data gravitasi didapatkan beberapa titik yang memiliki kemenerusan nilai FHD maksimum dan SVD nol yang diduga sebagai struktur berupa struktur F1 yang diduga merupakan sesar Derewo yang mengontrol mineralasisasi di Lapangan Wabu dan Struktur F2, F3, F4, dan F5 yang diduga merupakan patahan minor di lokasi penelitian. Berdasarkan intepretasi data resistivity-IP didapatkan empat zona prospek mineralisasi Emas.yang dicirikan dengan nilai respon IP tinggi sebesar 60-80 mrad yang diduga disebabkan oleh keterdapatan mineral sulfida yang konduktif. Korelasi antara data gravitasi dan resistivityIP didapatkan dua zona prospek mineralisasi yang direkomendasikan untuk dilakukan pengeboran untuk pengujian. Zona prospek tersebut adalah zona prospek P2 dan P4 yang memiliki nilai anomali gravitasi tinggi yang berasosiasi dengan garnet magnetite skarn dan respon IP tinggi yang berasosisasi dengan mineral sulfida. ......The Wabu Field is a gold mineralization prospect area located in Intan Jaya Regency, Central Papua. Further investigation needs to be carried out to strengthen evidence of the existence of a prospect zone for gold mineralization in the area prior to mining. Gravity and resistivity-IP methods are used to determine the presence of geological structures and distribution patterns of gold mineralization in the Wabu field. In this study, the GGMplus gravity data was processed to obtain a residual anomaly map which was then filtered by FHD and SVD. Based on FHD and SVD analysis on the gravity data obtained at several points that have continuity of maximum FHD and zero SVD values that are identified as structures, namely structure F1 which is suspected to be the Derewo fault which controls mineralization in the Wabu Field and structures F2, F3, F4, and F5 which are identified as minor faults at the study site. Based on the Interpretation of the resistivity-IP data, four gold mineralization prospect zones are identified. These are characterized by a high IP response value of 60-80 mrad which is thought to be caused by the presence of conductive sulphide minerals. Correlation between gravity and resistivity-IP data identified two gold mineralization prospect zones recommended for drilling for testing. These prospect zones are prospect zones P2 and P4 which have high gravity anomaly values associated with magnetite garnets skarn and high IP responses associated with sulfide minerals.