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INKLUSI FLUIDA DAN TIPE DEPOSIT MINERAL DI ARINEM CISEWU, KABUPATEN GARUT, JAWA BARAT Heru Sigit Purwanto
Jurnal Ilmiah Geologi PANGEA Vol 7, No 1 (2020): Jurnal Ilmiah Geologi PANGEA
Publisher : PROGRAM STUDI TEKNIK GEOLOGI FAKULTAS TEKNOLOGI MINERAL UPN "VETERAN" YOGYAKARTA

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Abstract

Sari - Kabupaten Garut, terutama daerah Arinem dan sekitarnya secara umum disusun oleh batuan beku yangberasal dari aktivitas magmatik tua dan gunung api muda Papandayan, hal ini menyebabkan adanya adanyapotensi cebakan mineral bijih. Daerah Arinem Cisewu dan sekitarnya merupakan daerah alterasi danmineralisasi diantaranya emas, tembaga, plumbum dan zink ( Heru Sigit dkk, 2019). Keberadaan satuanbatuan hasil dari proses vulkanisme purba berupa sedimen vulkanik dan intrusi, serta proses – proses geologilainnya yang mendukung terjadinya proses deposit mineral bijih. Lokasi penelitian menunjukan adanyakeberadaan struktur geologi yang mengontrol potensi endapan mineral bijih di daerah tersebut. Daerahtelitian termasuk dalam Ijin Usaha Pertambangan Perusahaan Tambang Aneka Tambang dan terdapat jugatambang rakyat yang sudah tutup mereka mengambil bijih emas, tembaga dan galena. Penelitain sebelumnyamenunjukkan bahwa daerah telitian dan sekitarnya merupakan tipe deposit Epithermal Low Sulfidation yangsecara umum keberadaannya pada urat-urat kuarsa (Antam, 2016 & Heru Sigit dkk,2019). Penelitian inimerupakan kelanjutan untuk mengetahui temperatur mineralisasi dan zona alterasi, disamping litologi danstruktur yang ada di daerah telitian. Metode secara umum penelitian adalah pemetaan geologipermukaan,sedangkan untuk mengetahui temperatur dengan menggunakan analisa fluid inclusion pada contohurat kuarsa yang diambil pada daerah telitian, Penelitian ini peneliti terdapat 4 sampel urat kuarsa akan tetapiyang bagus untuk dianalisa adalah 2 sampel yang diinterpretasikan dapat mewakili temperatur kehadiranmineralalisasi di daerah telitian, Hasilnya menunjukkan bahwa mineralisasi di daerah telitian diinterpretasikandengan temperatur berkisar antara 231OOC – 420C. Kata-kata kunci : mineral bijih, alterasi, mineralisasi, epithermal low sulfidation, inklusi fluida, urat kuarsa 
Rock slope kinematics analysis by Markland method of the Bener District, Purworejo Regency, Central Java, Indonesia Sari Bahagiarti Kusumayudha; Azwar Thamrin; Heru Sigit Purwanto
International Journal of Advances in Applied Sciences Vol 12, No 2: June 2023
Publisher : Institute of Advanced Engineering and Science

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.11591/ijaas.v12.i2.pp111-120

Abstract

Bener District, Purworejo Regency, Central Java, Indonesia, located in the Kulon Progo Mountains can be classified as a high-risk area. Many experts and researchers have studied landslides, but there has been little research on rock slope kinematics. In fact, when such a rock slope is unstable and poorly monitored, it has the potential to endanger the community or facilities at the adjacent site. This is why slope kinematics research is required. To complete this study, rock kinematics analysis using the Markland method was performed on six representative slopes. The assessment results show that Kaliwader slope A, Kaliwader slope B, and Argosari slope each tend to collapse with wedge failure, Kaliwader slope D and Wadas slope have the potential for wedge failure and planar slide, but Kaliwader slope C does not. Despite their steep inclination, slopes that are likely to fail are strongly related to the presence of geologic structures, particularly joints, and faults, at the sites. The findings of this study will be helpful in the development of landslide vulnerability zones in the context of disaster mitigation.
Pengaruh Kehadiran Airtanah Terhadap Kerentanan Gerakan Massa di Daerah Kenalan dan Sekitarnya, Jawa Tengah Siahaan, Boi Haris; Kusumayudha, Sari Bahagiarti; Purwanto, Heru Sigit
Jurnal Ilmiah Geologi PANGEA Vol 11, No 1 (2024): Jurnal Ilmiah Geologi Pangea
Publisher : PROGRAM STUDI TEKNIK GEOLOGI FAKULTAS TEKNOLOGI MINERAL UPN VETERAN YOGYAKARTA

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.31315/jigp.v11i1.11228

Abstract

Daerah penelitian termasuk dalam wilayah desa Kenalan, Kecamatan Borobudur, Kabupaten Magelang, berada pada koordinat 110o11’05”-110o14’15” BT dan 7o37’45”-7o40’05”LS, morfologi lereng datar hingga curam, sehingga rawan terhadap bencana gerakan massa. Batuan tersusun atas Satuan breksi andesit Kaligesing, Satuan lava andesit Kaligesing, Satuan batugamping Jonggrangan, Satuan endapan koluvium, dan Satuan endapan alluvial. Tujuan penelitian adalah melakukan analisis pengaruh keberadaan airtanah terhadap kejadian gerakan massa, menentukan faktor meamanan lereng yang berpotensi longsor, dan menyusun peta kerentaan gerakan massa di daerah penelitian. Metode penelitian menggunakan pendekatan kualitatif, kuantitatif, dan survey lapangan.  Analisis kestabilan lereng dilakukan terhadap 6 lereng, dengan hasil 3 lereng stabil, dan 3 lereng labil. Dari zonasi kerentanan gerakan massa, didapatkan 3 zona kerentanan. Zona dengan tingkat kerentanan rendah menempati 30% lokasi penelitian dengan muka airtanah berada pada kedalaman >20, dan terdapat 6 kejadian longsor. Tingkat kerentanan sedang menempati 45% lokasi penelitian dengan muka airtanah berada pada kedalaman 7-25m, dan terdapat 21 kejadian longsor. Tingkat kerentanan tinggi menempati 25% lokasi penelitan dengan kedalaman muka airtanah berada pada kedalaman <7m, dan terdapat 38 kejadian longsor. Muka airtanah berperan besar dalam menurunkan nilai faktor keamanan lereng. Proporsi kejadian longsor banyak terjadi pada daerah dengan muka airtanah rendah/dangkal dan pada sistem akuifer antar butir.
Stereographic for Development of Stricture Pattern of Geological Alteration Zone in Atauro Island, Timor-Leste Gomes, Nazario; Sutarto, Sutarto; Soesilo, Joko; Purwanto, Heru Sigit; Christophe, James
Asian Journal of Social and Humanities Vol. 2 No. 6 (2024): Asian Journal of Social and Humanities
Publisher : Pelopor Publikasi Akademika

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.59888/ajosh.v2i6.274

Abstract

The geological structural patterns and hydrothermal alteration zones of Atauro Island, Timor-Leste, which are influenced by the collision mechanism between the Banda Arc and the Australian Continent, are the subject of this study. The study identifies fault types and alteration zones through stereographic analysis. It indicates the possibility of mineralization in the area. Four alteration zones were identified in this study: argillic, Propylitic, calcosite, and geotite. The analysis results show that left-striking and normal faulting were essential in forming these zones. The mineralization zones, mainly chalcopyrite and chalcocite, are related to the north-northeast trending left horizontal Fault. In addition, this study suggests additional research that includes mineralogy, geochemical, and geophysical analyses to understand more about the characteristics of hydrothermal alteration zones and possible mineralization on Atauro Island. The results of this study are expected to improve our understanding of mineral resources in the region, and it is suggested that this information be considered by authorities responsible for the management of potential natural resources on Atauro Island, Timor.
ALTERATION AND GOLD MINERALIZATION PANINGKABAN AREAS GUMELAR SUB-DISTRICT, BANYUMAS REGENCY, CENTRAL JAVA PROVINCE Purwanto, Heru Sigit; Riswandi, Herry
Journal TECHNO Vol. 1 No. 1 (2015)
Publisher : Universitas Pembangunan Nasional Veteran Yogayakarta

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.31315/journal techno.v1i1.1504

Abstract

The research location is located in Paningkaban area and its surrounding areas that included in the areaof Gumelar Subdistrict, Banyumas Regency, and Central Java Province. The objective of the researchwas to show the presence of any structural geology control on research area that affect the distributionpatterns of quartz vein and gold/ore mineralization.The methodology in this research begins with data collecting process, which this preliminary data is thenbeing compiled to determine the next phase of the study. This study covers the geomorphology,stratigraphy, any structural and alteration mineralization observation. The geomorphology of the studyarea composed of the four original forms: volcanic, structural, karsts and fluvial form. The stratigraphycomposed of seven unclassified litho units and two litodem, namely (from old - young): Halang volcanicbreccias unit, Halang sandstone unit, Kumbang andesite lava unit, Tapak volcanic breccias unit, Tapaksandstones, unit Tapak limestone unit, alluvial deposits, and andesite intrusion.Hydrothermal alterations formed in the research area are carefully grouped into three types of alterationzoning and they are argillic alteration, propylitic alteration, and sub-propylitic alteration. Themineralization then is carefully classified as pyrite (FeS2), chalcopyrite (CuFeS2), galena (Pbs), bornite(Cu5FeS4). The macroscopic analysis of the structure in the study area based on the alignment of allegedtraces of the geological structure in the form of fault, or directions of the fold axis alignment, obtainedthe general alignment directions trending N 305° E (NW - SE), and N 055° E (NE - SW).In the research area, the mineralization process is controlled by geological structure such as fault andjoint. The appearance of the mineralization is abundant and can be found many fulfilling the joint zonemainly shear joint trending Northeast - Southwest and Northwest - Southeast, the direction of jointsharpness measured in the field relatively trending North - South. This study will emphasize on themeasurement and detailed analysis to know more about the gold mineralization process and otherminerals controlled by structures patterns. The structural control analysis can really be a good helpinghand in locating the mineralized areas because basically the activity and geological structure controlprocess are corridor for magma and the its rest compound that brings minerals, so the methods ofmineral ores exploration by structure control can be used in determining ore gold mineralized depositsprecipitate on gold deposits system and other minerals on a different area.Keywords: lithostratigraphy, structure, zone of opening, zone of alteration, mineralization, metalminerals
OPTIMIZATION OF PUMPING AND WATER FILTRATION FOR SUBTERRANEAN RIVER OF GOA TUK SARINING KEMBANG IN THE INTEREST OF WATER FULFILLMENT IN GEBANG HAMLET AND ITS SURROUNDING Purwanto, Heru Sigit; Sugiarto, Bambang; Fatchurohman, Dedi
Journal TECHNO Vol. 6 No. 1 (2020): November
Publisher : Universitas Pembangunan Nasional Veteran Yogayakarta

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.31315/journal techno.v6i1.4223

Abstract

Water is the primary needs for the livelihood of people in Gebang hamlet, Girisuko village, Gunung Kidul Regency, Special Region of Yogyakarta. Gebang is a hamlet in Panggang district, Gunug Kidul Regency, of which water supply is insufficient to meet the needs. There are 170 households with an average of 4 lives each, thus about approximately 680 people don’t have sufficient water supply. Water supply to the hamlet is constrained by the pumping ability.The neighborhood rely on overflowing raw water in high rainfall season that is channelled through pipe to the certain water tank prepared as reserves for dry season and few of them had used water from a cave. However, the pump is now broken so in a long dry season they need to buy water using tank truck. Based on the observation, this research planned to design water pump arrangement with high capacity so water can easily be channeled to the water tank and distributed to people in the neighborhood.The material absorbed in karst medium is related to each other, between organic (coliform parameter) and anorganic material (TDS parameter). The water puryfying process was conducted in laboratory and another process engaging gravity sand filter was chosen using zeolith with thickness of 40-50 cm that is able to decrease TDS from 232 – 268 ppm up to 180 ppm.
IMPLEMENTASI TEKNOLOGI PENGOLAHAN SAMPAH PLASTIK, KARET, DAN STYROFOAM SEBAGAI ENERGI ALTERNATIF Sugiarto, Bambang; Purwanto, Heru Sigit; Irfandi, Fauzan
Dharma: Jurnal Pengabdian Masyarakat Vol. 2 No. 1 (2021): Mei
Publisher : Universitas Pembangunan Nasional "Veteran" Yogyakarta

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.31315/dlppm.v2i1.4799

Abstract

Household waste, especially plastic, styrofoam and used tires, is a problem for the community because it reduces the quality of the environment. In addition, another problem faced by the community is the increase in household expenditure from consuming fuel for cooking. The community service team tries to overcome both of these problems by implementing waste-to-fuel processing technology. Community service activities include training, mentoring, and providing facilities for processing waste into environmentally friendly fuel. The activity was carried out at the Surolaras Waste Bank, Yogyakarta City. The benefits that are felt are reduced waste, fuel products that can be used for household needs, reduced household expenses, and a well-preserved natural environment.
Hydrothermal Alteration and Mineralization in the Grindulu River Segment, Pacitan, East Java: A Study of the Geotourism Potential of the River Area Mineralization Kurniawan, Oki; Purwanto, Heru Sigit; Harjanto, Agus; Winarno, Edy; Fatchurohman, Dedi; Pratomo, Septyo Uji
Journal of Applied Sciences, Management and Engineering Technology Vol 6, No 2 (2025)
Publisher : Institut Teknologi Adhi Tama Surabaya

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.31284/j.jasmet.2025.v6i2.8192

Abstract

The Grindulu River in Pacitan is one of the areas that exhibits manifestations of hydrothermal alteration and metal mineralization. However, the valuable metals found are relatively low, making it less economical to produce. This condition opens up other opportunities by utilizing the area as a natural laboratory for geological education and sustainable geotourism development. This study evaluates the potential for hydrothermal mineralization-based geotourism through geosite assessment. The study area comprises the Watupatok Formation and the Arjosari Formation, which show silicic, argillic, and propylitic alteration zones. The research methods include geological mapping, rock sampling, petrographic analysis, XRD, FA-AAS, and geosite assessment using the Kubalikova method, covering scientific, educational, aesthetic, and value-added aspects. The results show the presence of mineralization in the form of pyrite, chalcopyrite, sphalerite, and galena, with low levels of valuable metals (Au, Ag, Cu, Pb, Zn). Nevertheless, all three segments of the Grindulu River possess significant geosite value for educational and conservation purposes, with segment 2 considered the most ideal due to its superior accessibility and educational value. This study concludes that the Grindulu River is more appropriate for development as a sustainable geotourism destination based on conservation and geological education rather than mining exploitation.