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Pandiangan, Paiyan
"Pit Purnama merupakan salah satu prospek Tambang Emas Martabe yang berlokasi di Desa Aek Pining, Kecamatan Batangtoru, Kabupaten Tapanuli Selatan, Sumatera Utara dengan jenis endapan epitermal sulfidasi tinggi dan merupakan wilayah kerja PT. Agincourt Resources. Penelitian ini dilakukan untuk mengetahui sebaran litologi, alterasi dan mineralisasi emas yang selanjutnya akan dikelompokkan menjadi zona litologi, alterasi dan mineralisasi. Metode yang digunakan dalam penelitian ini adalah logging core, analisis petrografi irisan tipis, mineragrafi sayatan poles serta didukung data sekunder berupa data ASD (analitycal spectral device) dan data assay. Core logging terdiri dari 6 lubang bor yang terdiri dari 3 bagian XY, PQ, dan AB. Hasil penelitian ini menunjukkan litologi kawasan Pit Purnama terbagi menjadi 7 litologi, yaitu batuan andesit hornblend, dacite feldspar, breksi polimik kemasan terbuka, breksi polimik kemasan tertutup, andesit, dan batupasir dengan zonasi alterasi klorit ± kalsit, ilit ± smektit, silika ± sedikit ± alunite. ± kaolinit, dan silika dengan karakteristik kuarsa masif hingga tekstur vuggy. Zona mineralisasi emas dibagi menjadi 4 kelompok, yaitu sangat rendah (0 - 0,12 ppm), rendah (0,12 - 0,26 ppm), sedang (0,26 - 0,585 ppm), tinggi (> 0,585 ppm).

Pit Purnama is one of the prospects for the Martabe Gold Mine located in Aek Pining Village, Batangtoru District, South Tapanuli Regency, North Sumatra with high sulfidation epithermal deposits and is the working area of ​​PT. Agincourt Resources. This research was conducted to determine the distribution of lithology, alteration and mineralization of gold, which will then be grouped into lithology, alteration and mineralization zones. The method used in this research is the logging core, thin slice petrographic analysis, polishing cut mineragraphy and supported by secondary data in the form of ASD data (analitycal spectral device) and assay data. Core logging consists of 6 drill holes consisting of 3 sections XY, PQ, and AB. The results of this study indicate that the lithology of the Pit Purnama area is divided into 7 lithologies, namely hornblend andesite, dacite feldspar, open-pack polymic breccias, closed-pack polymic breccias, andesite, and sandstones with alteration zoning chlorite ± calcite, illite ± smectite, silica ± slightly ± alunite. ± kaolinite, and silica with the characteristics of massive quartz to vuggy texture. Gold mineralization zones are divided into 4 groups, namely very low (0 - 0.12 ppm), low (0.12 - 0.26 ppm), moderate (0.26 - 0.585 ppm), high (> 0.585 ppm)."
Depok: Fakultas Matematika dan Ilmu Pengetahuan Alam Universitas Indonesia, 2019
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UI - Skripsi Membership  Universitas Indonesia Library
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Safira Zulny
"Daerah penelitian “X” merupakan daerah prospek alterasi dan mineralisasi endapan emas yang termasuk dalam Zona Pegunungan Selatan Jawa bagian Timur. Penelitian ini bertujuan untuk mengetahui karakteristik alterasi dan mineralisasi endapan emas meliputi kehadiran himpunan mineral alterasi, mineral bijih, geokimia bijih, tekstur mineralisasi, persebaran zona alterasi hidrotermal, serta paragenesa endapan mineral bijih pada daerah penelitian. Pada penelitian ini, terdapat empat metode yang dilakukan meliputi petrografi, mineragrafi, XRD, dan AAS. Analisis petrografi dilakukan untuk mengamati karakteristik tekstur urat, mengidentifikasi kandungan mineral penyusun batuan dan keterdapatan himpunan mineral penciri zona alterasi hidortermal pada sampel batuan. Analisis XRD dilakukan untuk mengidentifikasi asosiasi mineral-mineral ubahan yang terbentuk pada zona alterasi di daerah penelitian yang sulit teridentifikasi melalui analisis petrografi. Analisis mineragrafi dilakukan untuk mengetahui karakteristik mineral bijih yang hadir, tekstur mineral bijih, keterdapatan mineral bijih yang berasoasiasi dengan endapan emas, serta penentuan paragenesa endapan mineral bijih pada daerah penelitian. Analisis AAS dilakukan untuk mengetahui keterdapatan unsur logam beserta kadar masing-masing unsur logam yang teridentifikasi pada daerah penelitian. Berdasarkan analisis petrografi dan XRD, zona alterasi hidrotermal yang berkembang pada daerah penelitian terdiri dari zona alterasi argilik dan propilitik. Zona alterasi argilik dicirikan oleh kehadiran mineral montmorillonite dan dickite dengan temperatur pembentukan diperkiran pada rentang suhu 200°-250°C. Zona alterasi propilitik dicirikan oleh melimpahnya kehadiran mineral klorit, epidot, dan kalsit dengan temperatur pembentukan diperkiran pada rentang suhu 120°-320°C. Berdasarkan analisis petrografi menunjukkan kehadiran tekstur urat pada daerah penelitian meliputi tekstur comb dan mosaic. Berdasarkan analisis mineragrafi, mineral bijih yang hadir di daerah penelitian meliputi mineral magnetit, pirit, kalkopirit, galena, rutil, ilmenit, hematit, kalkosit, goethite, dan hydrous iron oxide dengan tekstur mineral bijih berupa tekstur open space filling, diseminasi, penggantian, intergrowth, colloform, dan eksolusi. Berdasarkan analisis AAS, kehadiran emas ditunjukkan oleh terdeteksinya kadar unsur logam Au sebesar 0,09 - 2,5 ppm. Terdapat beberapa unsur logam lainnya yang teridentifikasi pada analisis AAS meliputi Cu, Pb, Zn, dan Ag. Mineral bijih yang berasosiasi dengan endapan emas pada daerah penelitian meliputi mineral pirit, kalkopirit, dan galena. Paragenesa endapan mineral bijih daerah penelitian terbagi menjadi dua tahap pembentukan yang diawali oleh terbentuknya mineral primer pada tahap hipogen meliputi mineral magnetit, pirit, kalkopirit, galena, rutil, dan ilmenit serta dilanjutkan oleh terbentuk mineral sekunder pada tahap supergen meliputi mineral hematit, kalkosit, goethite, dan hydrous iron oxide. Berdasarkan karakteristik alterasi dan mineralisasinya daerah penelitian termasuk dalam sistem endapan porfiri dan epitermal sulfidasi rendah.

Research area "X" is a prospect area for alteration and mineralization of gold deposits which is included in the Southern Mountain Zone of Eastern Java. This research aims to determine the characteristics of alteration and mineralization of gold deposits including the presence of alteration mineral assemblages, ore minerals, ore geochemistry, mineralization texture, distribution of hydrothermal alteration zones, as well as the paragenesis of ore mineral deposits in the research area. In this research, four methods were used including petrography, mineragraphy, XRD, and AAS. Petrographic analysis was carried out to observe the texture characteristics of the veins, identify the mineral content that makes up the rock, and the presence of mineral assemblages that characterize hydrothermal alteration zones in the rock samples. XRD analysis was carried out to identify alteration mineral associations formed in alteration zones in the research area that are difficult to identify through petrographic analysis. Mineragraphic analysis was carried out to determine the characteristics of the ore minerals present, the texture of the ore minerals, the presence of ore minerals associated with gold deposits, as well as determining the paragenesis of ore mineral deposits in the research area. AAS analysis was carried out to determine the presence of metal elements and the levels of each metal element identified in the research area. Based on petrographic and XRD analysis, the hydrothermal alteration zone that develops in the research area consists of argillic and propylitic alteration zones. The argillic alteration zone is characterized by the presence of montmorillonite and dickite minerals with formation temperatures estimated to range from 200°-250°C. The propylitic alteration zone is characterized by the abundant presence of chlorite, epidote, and calcite minerals with formation temperatures estimated to range from 120°-320°C. Based on petrographic analysis, it shows the presence of vein textures in the study area including comb and mosaic textures. Based on mineragraphic analysis, the ore minerals present in the research area include magnetite, pyrite, chalcopyrite, galena, rutile, ilmenite, hematite, chalcocite, goethite, and hydrous iron oxide with the ore mineral textures shown including open space filling, dissemination, replacement, intergrowth, colloform, and exsolution. Based on AAS analysis, the presence of gold was indicated by the detection of Au metal element levels of 0.09 - 2.5 ppm. There are several other metal elements identified in AAS analysis including Cu, Pb, Zn, and Ag. The ore minerals associated with gold deposits in the research area include pyrite, chalcopyrite, and galena. The paragenesis of ore mineral deposits is divided into two stages, starting with the formation of primary minerals at the hypogene stage including magnetite, pyrite, chalcopyrite, galena, rutile and ilmenite and continued by the formation of secondary minerals at the supergene stage including hematite, chalcocite, goethite, and hydrous iron oxide. Based on the characteristics of alteration and mineralization, the research area is classified within the porphyry and low-sulfidation epithermal deposit systems."
Depok: Fakultas Matematika dan Ilmu Pengetahuan Alam Universitas Indonesia, 2024
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UI - Skripsi Membership  Universitas Indonesia Library
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Ritonga, Bastian
"Pertambangan emas secara tradisional di Kecamatan Huta Bargot, Mandailing Natal, Sumatera Utara telah dilakukan + 12 tahun terakhir. Tujuan penelitian ini adalah untuk mengetahui hubungan antara karakteristik lingkungan (kadar merkuri air) dan karakteristik responden (umur, lama tinggal, lama kerja, lama berkerja/hari) dengan kadar merkuri rambut pekerja tambang emas tradisional di kecamatan Huta Bargot. Penelitian ini dilaksanakan di 6 desa yaitu Desa bangun sejati, Desa Binanga, Desa Hutabargot setia, Desa Hutarimbaru, Desa Kumpulan setia dan Desa Huta Bargot Nauli pada bulan Maret 2019 dengan desain cross sectional terhadap 60 orang pekerja tambang emas tradisional. Untuk memilih sampel terpilih digunakan metode quate sampling dengan jumlah sampel tiap desa sebanyak 10 orang Sampel dari tiap desa dipilih menggunakan metode purposive sampling. Kadar merkuri rambut pekerja masih dalam ambang baku mutu dengan rata-rata kadar merkuri 0,2117 µg/g. Dari 6 sampel air sungai yang diperiksa, 3 sampel air berada di atas baku mutu (> 0,001 mg/L ). Dari hasil analisis bivariat menunjukkan hubungan lama tinggal dengan kadar merkuri rambut. Hasil analisis multivariat diperoleh hubungan antara lama tinggal dengan kadar merkuri pada rambut (nilai p = 0,034)dengan OR=10,737 yang artinya pekerja tambang emas yang lama tinggal > 20 tahun memiliki peluang memiliki kadar merkuri rambut > 0,24 µg/g dibandingkan pekerja tambang yang lama tinggal < 20 tahun.

Traditional gold mining in Huta Bargot Subdistrict, Mandailing Natal, North Sumatra has been carried out  the last 12 years. The purpose of this study was to determine the factors that influence the mercury levels of traditional gold mine workers in the Huta Bargot sub-district. The research was carried out in 6 villages, bangun sejati, Binanga, Hutabargot setia, Hutarimbaru, Kumpulan setia and Huta Bargot Nauli Village in March 2019 with a cross sectional design for 60 traditional gold mining workers. To select the selected sample, the quate sampling method was used with a total sample of 10 villages. Samples from each village were selected using the purposive sampling method. Workers' mercury levels are still within the threshold of quality standards with an average mercury level of 0.2117 µg / g. 3 of 6 water samples were above the quality standard (> 0.001 mg / L). From the results of bivariate analysis shows the length of stay with hair mercury levels. The results of multivariate analysis found a relationship between length of stay with mercury levels in hair (p value = 0,034) with OR = 10.737, which means gold miners who live> 20 years have the opportunity to have a hair mercury level of > 0.24 µg / g compared to miners <20 years."
Depok: Fakultas Kesehatan Masyarakat Universitas Indonesia, 2019
T52671
UI - Tesis Membership  Universitas Indonesia Library
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Muhammad Rizhkal
"Pertambangan emas di kabupaten Mandailing Natal sudah ada sejak 2008. Tetapi semakin marak pada tahun 2010 di kecamatan Hutabargot dan di kecamatan Nagajuang pada November 2011. Tujuan dari penelitian ini adalah untuk menganalisis hubungan antara kadar merkuri pada rambut pada pekerja tambang terpajan merkuri dan karakteristik individu pekerja(usia, lama tinggal, status gizi dan konsumsi ikan) dengan gangguan keseimbangan tubuh. Penelitian ini menggunakan metode cross sectional. Data yang digunakan yaitu data primer dari kuesioner dan sekunder dari hasil uji laboratorium rambut. Sampel penelitian ini disesuaikan dengan sampel dari data sekunder yang menggunakan rumus Lemeshow sehingga didapatkan sampel 60 orang.
Hasil penelitian ini didapatkan tidak ada hubungan yang signifikan antara variabel independent (merkuri dalam rambut) dan variabel konfounding terhadap variabel dependent (gangguan keseimbangan tubuh). Walaupun hasil penelitian tidak menunjukkan hubungan yang signifikan jika dilihat dari nilai OR variabel merkuri dalam rambut masih tergolong tinggi yaitu 6,0 dan setelah dikontol variabel karakteristik individu OR merkuri dalam rambut turun menjadi 4,92.

Gold mining in Mandailing Natal regency has been around since 2008. But it became more prevalent in 2010 in Hutabargot sub-district and in Nagajuang sub-district in November 2011. The purpose of this study was to analyze the relationship between mercury levels in hair in mercury exposed workers and individual characteristics of workers (age, length of stay, nutritional status and consumption of fish) with body balance disorders. This study uses a cross sectional method. The data used are primary data from questionnaires and secondary from the results of hair laboratory tests. The research sample was adjusted to the sample from secondary data using the Lemeshow formula so that sample of 60 people was obtained.
The results of this study found that there was no significant relationship between independent variables (mercury in hair) and confounding variables on the dependent variable (body balance disorder). Although the results of the study did not show a significant relationship when viewed from the OR variable value of mercury in the hair was still relatively high at 6.0 and after being contracted the individual characteristic variable OR mercury in the hair dropped to 4.92."
Depok: Fakultas Kesehatan Masyarakat Universitas Indonesia, 2019
T53785
UI - Tesis Membership  Universitas Indonesia Library
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Mohammad Arief Ismanto
"ABSTRAK
Industri pertambangan emas sekarang ini mengalami berbagai tantangan di tengah situasi ekonomi global yang melemah, harga bahan produksi tambang yang relatif pada posisi di level bawah dan kesulitan menemukan cadangan berkadar emas tinggi di dekat permukaan.Cadangan bijih emas tipe sulfidasi tinggi merupakan pilihan yang ekonomis dengan kadar emas relatif rendah hingga menengah cut-off 0.3 g/t hingga 0.5 g/t namun memiliki bulk-density yang luas. Cadangan emas tipe sulfidasi tinggi dengan level ketebalan bijih oksidasi yang signifikan 70m-125m akan menjadikan suatu bisnis penambangan yang menguntungkan. Hal ini dikarenakan proses metalurgi ekstraksi emas dapat dilakukan dengan metode cyanide-leach yang biaya produksinya relatif murah dibanding proses-proses ekstraksi emas lainnya.Walaupun ekonomis dan berbiaya murah, namun penambangan cadangan bijih emas tipe sulfidasi tinggi ini memiliki beberapa tantangan seperti genesa mineralisasi sulfidasi tinggi yang memiliki zonasi bijih mengandung alterasi mineral clay lempung yang menghambat proses irigasi cyanide leach liquid, asosiasi dengan mineral sulfida dan adanya gangue mineral mengandung tembaga Cu yang akan bereaksi dengan sianida membentuk kimiawi komplek Cu-Cn sehingga meningkatkan konsumsi sianida.Studi Geometalurgi yang menggabungkan analisis mikro petrologi terkait mineralogi, tekstur bijih dan mineral gangue dengan berbagai variasi uji metalurgi dan pengelompokan domain bijih dengan bantuan teknologi spectrometer akan membantu mengantisipasi kendala dan meningkatkan optimisasi metalurgi ekstraksi bijih emas

ABSTRACT
The gold mining industry is currently facing challenges amid a weakening global economic situation, relatively low prices of mining production materials and the difficulties in finding high grade gold deposits near the surfaceHigh sulfidation gold ore deposits are an economical choice with relatively low to medium grade gold cut off 0.3 g t up to 0.5 g t but have large bulk density. High sulfidation gold deposits with significant oxidation ore thickness levels 70m 125m will make a profitable mining business. This is because the metallurgical process of gold extraction can be processed by cyanide leach method which is relatively cheap production cost compared to other gold extraction processes.Although economical and low cost, this high sulfidation gold ore reserve has some challenges in extraction such as high sulphidation mineralization origin that have ore zonation containing mineral clay alteration that inhibits the cyanide leach liquid irrigation process, associated with sulphide minerals and the presence of mineral gangue containing copper Cu which will react with cyanide to form Cu Cn complex chemicals thus increasing cyanide consumption.Geometallurgical studies that combine mineralogy related petrology analyzes, ore textures and gangue minerals with varying metallurgical test and ore domain groupings with the help of spectrometer technology will help to anticipate constraints and improve metallurgical optimization of gold ore extraction"
2017
T47865
UI - Tesis Membership  Universitas Indonesia Library
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Ivan Aulia Azhari
"Realisasi penerimaan Pajak Bumi dan Bangunan Perdesaan dan Perkotaan PBB-P2 di Kabupaten Tapanuli Selatan mengalami penurunan setelah penerapan PBB Online. Hal ini bertolak belakang dengan tujuan penerapan kebijakan tersebut yaitu untuk meningkatkan penerimaan PBB-P2. Penelitian ini bertujuan untuk mendeskripsikan implementasi PBB-P2 dan hambatannya. Penelitian menggunakan pendekatan kualitatif dengan teknik pengumpulan data wawancara mendalam.
Hasil penelitian ini menunjukkan bahwa implementasi PBB-P2 di Kabupaten Tapanuli Selatan dijalankan oleh BPKPAD bekerjasama dengan pihak kecamatan, kelurahan, desa, dan Bank Sumut. Hambatan dalam implementasi PBB-P2 diantaranya SDM kurang memadai, sulitnya pengawasan, kepatuhan Wajib Pajak rendah, NJOP yang belum update, dan pengaruh faktor politik.

Realization of land and building tax Rural and Urban revenues in Kabupaten Tapanuli Selatan decreased after the adoption of the PBB Online. This is in contrast to the objective of implementing the policy that is to increase revenue. This study aims to describe the implementation of land and building tax Rural and Urban and its constraints. The study used a qualitative approach with in depth interview data collection techniques.
The results of this study indicate that the implementation of land and building tax Rural and Urban in Kabupaten Tapanuli Selatan run by BPKPAD in cooperation with the sub district, village, village, and Bank Sumut. Obstacles in the implementation of land and building tax Rural and Urban include insufficient human resources, difficulty of supervision, low taxpayer compliance, NJOP that has not been updated, and the influence of political factors.
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Depok: Fakultas Ilmu Sosial dan Ilmu Politik Universitas Indonesia, 2017
S67171
UI - Skripsi Membership  Universitas Indonesia Library
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Reniastoetie Djojoasmoro
"Sumatran orangutans, found in the Province of Nangroe Aceh Darussalam and North Sumatra Province, are fragmented into four populations. One of these populations exists in Angkola, a forested area located in the southern part of Lake Toba. This population is considered small and narrowly distributed. Our survey shows that individual orangutans appear in and around the Dolok Sibualbuali Nature Reserve. This indicates that orangutans can adapt to fragmented habitats, such as those found near Dolok Sibualbuali Nature Reserve, south of Tapanuli, North Sumatra.
The preliminary study was conducted from April 2002 to January 2003. This study recorded the distribution and daily activities of orangutans in Dolok Sibualbuali Nature Reserve. Repeated crisscrossing surveys and focal animal observation were used to document orangutan distribution and daily activity.
Human activities are the main factor for the loss of orangutan habitat. Illegal logging, forest conversion for timber concessions and plantations, road construction, and settlement are the main factors for forest loss. This forces orangutans out of their native habitat and makes them vulnerable to extinction.
Based on direct sightings, orangutans are found at Aek Nabara and Sitolu. Moreover, the presence of orangutans is indicated by nests at the Sihulambu and Bulu Mario sites. The orangutan population is not evenly distributed but seems to be present at locations with food resources.
Seven individuals were chosen as focal animals. They consisted of three adult females, three sub-adult males, and one juvenile. Total observation time was 757 hours and 40 minutes. Feeding, moving, resting, nesting, and social activities were the main activities that were recorded. Orangutans spent their daily activity budgets as follows: feeding (42.29%), moving (16.47%), resting (37.41%), nesting (1.89%), and social contact (1.93%). Orangutans spent much of their time (42.29%) feeding, particularly when food resources were abundant. Due to their large body size, food consumption was high.
There are 115 types of orangutan food consisting of fruits (36.6%), flowers (3.89%), leaves (28.33%), bark (17.7%), and pith/stem (11.67%), and other food types (insects, honey, etc.) (1.67%). Fruit is the main source of orangutans' food.
We concluded that the distribution and daily activity of orangutans at Dolok Sibualbuali Nature Reserve are greatly influenced by the availability of food, particularly fruit. When favored fruit is abundantly available, orangutans will constantly consume that fruit and visit fruit trees of the same species in other locations. Orangutans will also search for other food in community farms near the Nature Reserve when forest fruit availability is low, leading to conflict with local people."
Depok: Universitas Indonesia, 2004
T11674
UI - Tesis Membership  Universitas Indonesia Library
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Azky Ramaniya Sukardi
"Daerah penelitian terletak pada Pulau Seram merupakan salah satu wilayah yang memiliki potensi prospek komoditas emas dikarenakan ditemukannya indikasi mineralisasi emas. Hal ini juga dikorelasikan berdasarkan penelitian sebelumnya bahwa daerah penelitian merupakan endapan emas orogenik. Subjek utama penelitian ini adalah conto sedimen sungai aktif. Penelitian ini dilakukan menggunakan analisis statistik dan geologi. Analisis statistik dilakukan untuk mengetahui sebaran anomali dan juga asosiasi unsur yang terdapat pada daerah penelitian. Sedangkan untuk analisis geologi dilakukan dengan mengintegrasi conto sedimen sungai aktif dan conto konsentrat dulang yang berasal dari PSDMBP dengan melakukan analisis petrografi, morfografi dan morfometri  Hasil penelitian menunjukkan persebaran anomali yaitu Cu, Pb, Zn, Fe, Mn, Li, Co, Na, Bi, Sr dan Ba sebesar 44.255ppm, log 1.900ppm, 148.605ppm, 4.734ppm, log 3.189ppm, 27.302ppm, 41.374%, 7609.713ppm, 53.807ppm, log 1.480ppm, log 1.592ppm, 184.198ppm, log 1.924ppm dan 263.139ppm. Berdasarkan analisis multivariat, didapatkan 4 kelompok asosiasi unsur yaitu : Cu-Zn-Rb-Ba-(Fe), Cu-Co-Fe, Na-Sr dan Fe-Mn. Unsur yang digunakan sebagai pathfinder untuk deposit emas adalah unsur Cu, Pb, Zn, Fe, Mn, Na, Bi, Co, W, Rb, Sr dan Ba sehingga terdapat 4 daerah prospek pada daerah penelitian. Persebaran anomali pada daerah penelitian diinterpretasikan terjadi akibat faktor geologi berupa transportasi, erosi, serta pelapukan dari litologi dan mineral bijih yang terdapat pada daerah penelitian.

The research area, Seram Island, is one of the areas that has potential prospects for the commodity gold due to the indications of gold mineralization were found. This also correlated with based on previous research, the research area is an orogenic gold deposit. The main subject of this research is sediment stream samples. This research was conducted using statistic and geological analysis. Statistic analysis was carried out to determine the distribution of anomalies and also the elemental associations found in the study area. Meanwhile, geological analysis was carried out by integrating active river sediment samples and pan concentrate samples originating from PSDMBP by conducting petrographic, morphographic and morphometric analysis. The results showed an anomalous distribution of Cu, Pb, Zn, Fe, Mn, Li, Co, Na, Bi , Sr and Ba of 44.255ppm, log 1.900ppm, 148.605ppm, 4.734ppm, log 3.189ppm, 27.302ppm, 41.374%, 7609.713ppm, 53.807ppm, log 1.480ppm, log 1.592ppm, 184.198ppm, log 1.924ppm and 263.139ppm. Based on multivariate analysis, 4 groups of elemental associations were obtained, namely: Cu-Zn-Rb-Ba-(Fe), Cu-Co-Fe, Na-Sr and Fe-Mn. The elements used as pathfinder for gold deposit are the elements Cu, Pb, Zn, Fe, Mn, Na, Bi, Co, W, Rb, Sr and Ba ​​so that there are 4 prospect areas in the study area. The distribution of anomalies in the study area is interpreted to occur due to geological factors in the form of transportation, erosion, and weathering of lithology and ore minerals found in the study area."
Depok: Fakultas Matematika dan Ilmu Pengetahuan Alam Universitas Indonesia, 2022
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UI - Skripsi Membership  Universitas Indonesia Library
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Alpha Agustinus; Budi Sudiarto
"Perusahaan tambang sangat tergantung pada bahan bakar fosil untuk memenuhi kebutuhan listrik dan kegiatan
pertambangan seperti penggunaan alat berat. Oleh karena itu, emisi gas rumah kaca akibat pembakaran bahan
bakar fosil ini telah menjadi isu utama terkait dampak terhadap lingkungan akibat kegiatan pertambagan. Energi
terbarukan seperti Pembangkit Listrik Tenaga Surya (PLTS) dapat menjadi solusi alternatif untuk mengatasi
masalah tersebut. Penelitian ini bertujuan untuk meneliti bauran PLTS yang optimal pada pabrik pengolahan
mineral di tambang emas Newmont Suriname. Perangkat lunak HOMER digunakan untuk mendesain bauran
PLTS paling optimal. Perangkat lunak ETAP digunakan untuk menvalidasi desain secara teknis teknis melalui
analisis aliran daya dan analisis arus hubung singkat.

Mining companies are highly dependent on fossil fuels to meet their electricity needs and mining activities such
as the use of heavy equipment. Therefore, the greenhouse gas emissions due to burning of fossil fuels have become
a major issue related to the impact on the environment due to mining activities. Renewable energy such as
Photovoltaic (PV) can be an alternative solution to overcome this problem. This study aims to examine the optimal
penetration of Photovoltaic (PV) at Processing Plant Newmont Suriname gold mine. HOMER software is used to
design the most optimal Photovoltaic (PV) penetration. ETAP software is used for technical validation through
load flow and short-circuit analysis.
"
Jurnal Pendidikan Teknologi Kejuruan, 2023
Majalah, Jurnal, Buletin  Universitas Indonesia Library
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Tobing, Elisha Christy Rotua Br
"Kucing Liar (KL) merupakan endapan Cu-skarn terbesar dan signifikan di skala dunia yang terletak di Tembagapura, Papua, Indonesia. Endapan ini merupakan bagian dari wilayah penambangan PT. Freeport Indonesia yang telah beroperasi sejak tahun 1967, akan tetapi, sampai saat ini proses genesa atau pembentukan endapan Kucing Liar masih diperdebatkan apakah terbentuk akibat intrusi atau proses pensesaran karena ditemukan sebuah sesar besar yang memotong perlapisan di endapan ini. Untuk membantu menjawab pertanyaan tersebut, penulis melakukan penelitian pada area ini dengan menganalisis data yang didapat dari kegiatan core detailed logging dan core orienting dari 6 lubang bor yang representatif, yang dilanjutkan dengan menganalisis sayatan tipis untuk mengkonfirmasi hasil detailed logging. Interpretasi hasil penelitian secara singkat menyatakan bahwa deposit ini dihasilkan dari salah satu tubuh Grasberg Intrusion Complex (GIC) yang memotong batuan sedimen karbonatan berumur Kapur Akhir hingga Miosen. Lokasi intrusi tidak dapat diidentifikasi secara spesifik, tetapi diinterpretasi intrusi ini memotong stratigrafi mulai terdiri dari Kelompok Kembelangan (KG) sampai Kelompok Batugamping Papua New Guinea (PNGLG) yang lebih muda. Sistem hidrotermal yang berasal dari proses pembekuan intrusi magma kemudian menghasilkan alterasi skarn yang terpusat di interval bawah Formasi Batu Gamping Waripi (Tw1) dan interval atas Formasi Batu Gamping Ekmai. Sistem alterasi skarn juga merupakan host mineralisasi sulfida (pirit-kalkopirit-bornit-kovelit) yang mengandung bijih (ore) tembaga (Cu) yang merupakan objek tambang dari endapan ini. Alterasi skarn di area ini dibagi menjadi 9 zona berdasarkan asosiasi mineral alterasi yang terbentuk, sedangkan mineralisasi sulfida dikelompokkan menjadi 6 tipe (styles) berdasarkan kenampakan dan konsentrasinya. Tipe mineralisasi yang berbeda dihasilkan dari perbedaan porositas / permeabilitas batuan induk dan tingkat alterasinya. Endapan Kucing Liar juga dipotong oleh sesar naik bernama Sesar Idenberg No. 1, seperti yang telah disebutkan sebelumnya. Dampak proses pensesaran pada endapan Kucing Liar juga merupakan topik penelitian yang menarik yang terus dikaji semenjak eksplorasi sampai produksi guna membantu memperkirakan cadangan bijih dari endapan. Dalam makalah ini, analisis mengenai kontrol struktur besar terhadap sistem alterasi dan mineralisasi sulfida didasarkan pada zonasi alterasi yang telah dibuat penulis dan distribusi konsentrasi sulfida hasil logging dari keenam lubang bor. Untuk mendukung analisis kontrol struktur pada area ini, penulis juga menganalisis tren orientasi urat hidrotermal menggunakan bantuan perangkat lunak Dips. Analisis urat hidrotermal dilakukan terhadap 4 jenis urat, yaitu kalsit, kuarsa, anhidrit, dan sulfida, dan menunjukkan 3 tren pengendapan urat berbeda yang dipengaruhi oleh sifat formasi dan proses pensesaran

Kucing Liar (KL) is the biggest and significant Cu-skarn deposit around the world that is located in Tembagapura, Papua, Indonesia. This deposit is a part of PT.Freeport Indonesia mining area that has been operated since 1967, nonetheless, the generation process of Kucing Liar deposit is still being debated whether it was formed by the intrusion or by the late faulting process that is indicated from the presence of Idenberg Fault No.1. To help answering this question, the writer did a research in this area with data generated from core detailed logging and core orienting activity of 6 representative boreholes of this deposit, then the analysis is continued by analyzing the thin section of the samples. The recent and scientifically proven interpretation states that this deposit was generated from one of the Grasberg Intrusion Complex (GIC) that cut through the carbonaceous sedimentary rocks of Late Cretaceous to Miocene ages. The intrusion location can not be specifically identified but strongly believed had cut through the rocks of Kembelangan Group (KG) and Papua New Guinea Limestone Group (PNGLG). The hydrothermal system derived from the magma emplacement of intrusion then created the skarn alteration system that are mainly hosted in Lower Waripi Limestone Formatiom (Tw1) and Upper Ekmai Limestone Formation. The skarn alteration system has also been the host of sulphide mineralization (pyrite-chalcopyrite-bornite-covellite) that has been the ore of the deposit for its high Cu content. The skarn alteration is divided into 9 zonation based on their formed or altered mineral association, meanwhile the sulphide mineralization is grouped into 6 styles based on their appearence and concentration. The different styles are interpretated to be the function of host rock porosity/permeability and its degree of alteration. The Kucing Liar deposit is also cut by a thrust fault, named Idenberg Fault No. 1, as mentioned before. The impact of major faulting process on Kucing Liar deposit also has been an interesting research topic and continually analyze through time of exploration and production to help estimating the reserved ores. In this paper, this analysis is based on the the alteration zonation and the sulphide concentration distribution datas of 6 boreholes. To support the geological structure control analysis on this area, the writer also analyze the trend of hydrothermal vein orientation with the help of Dips software. The hydrothermal vein analysis from 4 types of vein, calcite, quartz, anhydrite, and sulphide, shows there are 3 trends of vein deposition orientation that were influenced by the formation properties and the late faulting process."
Depok: Fakultas Matematika dan Ilmu Pengetahuan Alam Universitas Indonesia, 2020
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