Temperature f Gold Mineralization In Tugurejo Area and Its Surrounding, Slahung Subdistrict, Ponorogo District, East Java Province, Indonesia

Authors

  • Heru Sigit Purwanto Geological Engineering of University Pembangunan Nasional Veteran Yogyakarta, Indonesia

Keywords:

sulfidation, alteration, mineralization, quartz, fluid inclusion

Abstract

Our research was conducted in Tugurejo Area and its surrounding, Slahung District, Ponorogo Regency, East Java, Indonesia. It consists of 2 informal lithostratigraphic units, that are the Watupatok Formation lava unit and the Watupatok Formation breccia unit. Tugurejo area and its surrounding is an area of alteration and mineralization, such as gold, copper and zinc (Purwanto, et al., 2021). The geological structures of the research site are predominantly joints filled with quartz veins and faults in the direction of NE-SW, NW-SE and E-W. The hydrothermal alterations formed in the research site were grouped into three alteration types, which are silica type (defined by Pyrite ± Quartz), argillic type (defined by Smectite ± Kaolinite ± Quartz ± Pyrite ± Albite), and propylitic (identified by Chlorite ± Albite ± Quartz ± Dolomite ± Pyrite ± Smectite ± Illite minerals). The mineralizations encountered at the research site are Pyrite (FeS2), Chalcopyrite (CuFeS2), Sphalerite (ZnS). Previous research showed that the area and its vicinity has Epithermal Low Sulfidation deposit type and Intermediate Sulfidation which generally could be identified in the quartz veins (Purwanto, et al,2021). This research is a continuation of the previous one in order to know the temperature of mineralization and alteration zone, as well as lithology and geological structure in research area. The general method of this research is surface mapping, and the temperature data was obtain by fluid inclusion analysis of the quartz vein samples acquired in the area. There are 2 samples of quartz to be analyzed and interpreted to represent the temperature of mineralization in the area. Based on the analysis result, we conclude that the temperature of mineralization in the research area is between 263°C - 312°C with salinity 5.13 – 6.13 wt% NaCl and 273 – 300OC, with salinity 3,16 - 4,24 %WT

References

. Arifudin Idrus and Esti Handayani, 2017.Geology and Characteristics of Low Sulfidation EpithermaVein in Sanepo area, East Java, Indonesia, Indonesia Mining Journal,No:1,oktober 2017,93-103

. Bateman, A.M., 1981., Mineral Deposit 3rd edition, Jhon Wiley and Sons, New York.

. Boyle,R.W., 1970. The Soure of Metal and Gangue Elements in Hydrothermal Deposits. International Union Geology Science. A.2. Stuttgart.

. Bunde, A. & S. Havlin.,1994. Fractals in Science, Springer Verlag, 298 hal.

. Corbett, G. J. dan Terry Leach. 1997. Southwest Pacific Rim Gold-Copper Systems: Structure, Alteration, and Mineralization. A workshop presented for the Society of Economic Geologist, Townsville.

. Craw.D., Windle,S.J and Angus,P.V. 1999. Gold mineralization without quartz veins in a ductile-brittle shear zone, Macraes Mine, Otago Schist, New Zaeland. Mineralium Deposita 34 : 382-394.

. Dagnew Girmay Nega., 2005. Au-Ag of Deposite Model supergen at epithermal quartz vein type in Pongkor, West Java. Doktor Program, ITB (unpublish ).

. Davis, B.K and Hippertt, J.F.M. 1998. Relationships between gold concentration and structure in quartz veins from the Hodgkinson Province, Northeastern Australia. Mineralium Deposita 33: 391-405.

. Harris, L.1988. Structural control of gold mineralization. Structural Geology Workshop Manual, Australia : Hermitage Holdings Pty,Ltd

. Heru Sigit Purwanto, Ibrahim Abdullah & Wan Fuad Wan Hassan. 2001. Structural control of gold mineralization in Lubok Mandi area, Peninsular Malaysia. International Geoscience Journal, Special Issue on Rodinia,Gondwana and Asia 4(4) :742-743.

. Heru Sigit Purwanto,Agus Harjanto, Dedi Fatuchurohman, 2021, Structural Control on Alteration and Gold Mineralization at Tugurejo Area Slahung Distric, Ponorogo regency, East Jawa Province. IOSR Journal of Engineering, ISSN € :2250-3021, ISSN (p) : 2278-8719, Vo; II pp31-38.

. Judith L.Hanah & Holly J.Stein. 1990. Magmatic and hydrothermal processes in ore-bearing systems. Geological Society of America Journal. Special Paper 246 : 1-10.

. Korvin, G., 1992, Fractal Models in Earth Sciences, Elsevier Science Publishers.

. Morrison, Gregg., Dong Guoyi, dan Sabhash Jaireth. 1990. Textural Zoning in Epithermal Quartz Veins. Australia: Klondike Exploration Services.

. Rickard, M. 1972. Fault Classification-Discussion. Bulletin Geology Society of America, Vol 105, hal 1-41.

. Samodra H, Gafoer S, Tjokrosapoetro S, 1992, Map of Pacitan Sheet , Jawa (Pacitan-1507-4): scale 1 : 100 000, Direktorat Geologi Indonesia

. Salma Difa Masti, Arifudin Idrus, 2019. Geology Alteration and Mineralization Ephitermal High Sulfidation in Wonokerto area Blitar Distrik, East Java, Indonesia, Seminar Nasional Kebumian ke 12, 5’6 September 2019

. Sillitoe, Richard H. dan J.W. Hedenquist. 2003. Linkages between Volcanotectonic Settings, Ore-Fluid Compositions, and Epithermal Precious Metal Deposits. Society of Economic Geologists Special Publication 10, hal 315-343.

. Van Bemmelen, R.W., 1949. The Geology of Indonesia, Volume I. The Hague Martinus Nijhoff, Netherland.

. White, N. C. dan J. W. Hedenquist. 1995. Epithermal Gold Deposits: Styles, Charecteristics and Exploration. Society of Economic Geologists 25, hal 1-13.

Downloads

Published

2022-04-30

How to Cite

Heru Sigit Purwanto. (2022). Temperature f Gold Mineralization In Tugurejo Area and Its Surrounding, Slahung Subdistrict, Ponorogo District, East Java Province, Indonesia. iJournals:International Journal of Software & Hardware Research in Engineering ISSN:2347-4890, 10(4). Retrieved from https://ijournals.in/journal/index.php/ijshre/article/view/103