@article{MAKHILLJEAS2017121314614,
    title = {Gold Mineralization in Paningkaban Areas Gumelar Sub-District,
Banyumas Regency, Central Java},
    journal = {Journal of Engineering and Applied Sciences},
    volume = {12},
    number = {13},
    pages = {3518-3522},
    year = {2017},
    issn = {1816-949x},
    doi = {jeasci.2017.3518.3522},
    url = {https://makhillpublications.co/view-article.php?issn=1816-949x&doi=jeasci.2017.3518.3522},
    author = {Dedi,Herry and},
    keywords = {mineralization,structure,alteration,Hydrothermal,deposits},
    abstract = {Hydrothermal alterations formed in the research area are carefully grouped into three types of
alteration zoning and they are argillic alteration, propylitic alteration and sub-propylitic alteration. The
mineralization then is carefully classified as pyrite (FeS<sub>2</sub> ), chalcopyrite (CuFeS<sub>2</sub> ), galena (Pbs), bornite (Cu<sub>5</sub>FeS<sub>2</sub> ). 
In the research area, the mineralization process is controlled by geological structure such as fault and joint. The
appearance of the mineralization is abundant and can be found many fulfilling the joint zone mainly shear joint
trending Northeast-Southwest and Northwest-Southeast, the direction of joint sharpness measured in the field
relatively trending North-South. This study will emphasize on the measurement and detailed analysis to know
more about the gold mineralization process and other minerals controlled by structures patterns. The structural
control analysis can really be a good helping hand in locating the mineralized areas because basically the
activity and geological structure control process are corridor for magma and the its rest compound that brings
minerals, so, the methods of mineral ores exploration by structure control can be used in determining ore gold
mineralized deposits precipitate on gold deposits system and other minerals on a different area.}
    }