2014 Vol. 47, No. 1
Article Contents

FAN Bao-cheng, LI Bao-qiang, JI Wen-hua, MENG Guang-lu, CAO Ji-fei, WANG Bin, ZHANG Jing, CAO Xin, LV Peng-rui, YANG Bo. Geological Characteristics and Significance of Makmal Gold Deposit, Kyrgyzstan[J]. Northwestern Geology, 2014, 47(1): 165-170.
Citation: FAN Bao-cheng, LI Bao-qiang, JI Wen-hua, MENG Guang-lu, CAO Ji-fei, WANG Bin, ZHANG Jing, CAO Xin, LV Peng-rui, YANG Bo. Geological Characteristics and Significance of Makmal Gold Deposit, Kyrgyzstan[J]. Northwestern Geology, 2014, 47(1): 165-170.

Geological Characteristics and Significance of Makmal Gold Deposit, Kyrgyzstan

  • The Makmal large-scale gold deposit, located in Middle Tianshan orogenic belt of Kyrgyzstan, belongs to the contact metasomatic type gold deposit of intermediate-acidic intrusions. The intermediate-acidic intrusive rocks are widely distributed in Xinjiang, where many gold deposits or occurrences are found developed within intermediate-acidic intrusions or their outer contact zone. Thus, the mineralization conditions and prospecting potential of this type of gold deposit are satisfied in Xinjiang, and three middle-scale gold deposits (such as Duonalasayi deposit) have been found there recently. However, this type of gold deposit is less in origin and small in scale. In this paper, the geological characteristics of Makmal large-scale gold deposit have been summarized to provide some help for prospecting this type of gold deposits in Xinjiang.
  • 加载中
  • 陈喜峰, 彭润民, 刘家军, 等.吉尔吉斯斯坦库姆托尔超大型金矿床地质特征[J].黄金地质, 2010, 31(12):15-19.

    Google Scholar

    Chen Xifeng, Peng Runmin, Liu Jiajun, et al.Geological characteristics of Kumtor super large gold deposit in Kyrgyzstan[J].GOLD, 2010, 31(12):15-19.

    Google Scholar

    杨富全, 毛景文, 王义天, 等.新疆西南天山金矿床主要类型、特征及成矿作用[J].矿床地质, 2007, 26(4):361-379.

    Google Scholar

    Yang Fuquan, Mao Jingwen, Wang Yitian, et al.Major types, characteristics and metallogeneses of gold deposits in southwest Tianshan Mountains, Xinjiang[J].Mineral Deposits, 2007, 26(4):361-379.

    Google Scholar

    陈衍景.为什么中酸性小岩体成大矿[J].西北地质, 2012, 45(4):128-133.

    Google Scholar

    Chen Yanjing.Why Small Granitic Stocks Associate with Giant Mineral Systems[J].Northwestern Geology, 2012, 45(4):128-133.

    Google Scholar

    何国琦, 李茂松, 刘德全, 等.中国新疆古生代地壳演化及成矿[M].新疆:新疆人民出版社, 1994.

    Google Scholar

    He Guoqi, Li Maosong, Liu Dequan, et al.China's Xinjiang Paleozoic crustal evolution and mineralization[M].Xinjiang People's Publishing House, Xinjiang, 1994.

    Google Scholar

    王作勋, 邬继易, 吕喜朝, 等.天山多旋回构造演化及成矿[M].北京:科学出版社, 1990.

    Google Scholar

    Wang Zuoxun, Wu Jiyi, LÜ Xichao, et al.Tianshan Tectonic Evolution and Mineralization of polycyclic[M].Science Press, Beijing, 1990.

    Google Scholar

    范堡程, 孟广路, 王斌, 等.吉尔吉斯塔拉斯-卡拉塔乌地块构造演化与成矿[J].西北地质, 2013, 46(2):54-62.

    Google Scholar

    Fan Baocheng, Meng Guanglu, Wang bin, et al.Micro-continent tectonic evolution of Talas-Kalataw in Northern Tianshan, Kyrgyzstan[J].Northwestern Geology, 2013, 46(2):54-62.

    Google Scholar

    Пак Н.Т..Формациии рудоносных метасоматитов Чаарташских гор[J].Бишкек: Илим, 1992, 102-124.

    Google Scholar

    Djenchuraeva R., Pak N., Sorokin T., et al. Gold Deposit Makmal and Model of Formation[J].NI, Moskow, 1999, (1):3-14.

    Google Scholar

    Djenchuraeva R., Pak N., Usmanov I.Gold deposit MakmalPaleozoic geodynamicsand intrusion-related Au deposits[J].Guide-book.London, 2001, (2):82-96.

    Google Scholar

    Додонова Т. А. Магматические формации Киргизииг[J].Труды управления геологии КирССР.-Фрунзе, 1974, (3):37-44.

    Google Scholar

    Стратифицированные и интрузивные образования Киргизии[J].Фрунзе. Илим, 1982, (1):370.

    Google Scholar

    Дженчураева Р.Д..Скарны Срединного Тянь-Шаня[J].Закономерности размещения и рудоносность.-ФрунзеИлим, 1983, 283.

    Google Scholar

    Пак Н.Т..Околорудные метасоматиты крупных месторождений золота Кыргызстана[J].Рудные провинции Центральной Азии. Доклады на МГК-33.-Осло, Алматы, 2008, 43-54.

    Google Scholar

    Дженчураева Р.Д..Pудоносные очагово-купольные структуры в Северном и Срединном Тянь-Шане[J]. Изв. АН СССР. 1990.Cер. геол., (4):126-135.

    Google Scholar

    Дженчураева Р.Д..Роль структур глубокого заложения в формировании крупных месторождений(на примереТянь-Шаня)[J].Известия НАН КР, 1999, 110-116.

    Google Scholar

    Дженчураева Р.Д.. Явления полигенности на месторождениях Срединного Тянь-Шаня[J]. Геология рудных месторождений, 1990, (1):59-72.

    Google Scholar

    Дженчураева Р.Д..Геодинамика металлогения и рудогенез (на примере Тянь-Шаня и прилегающих территорий)[M].Бишкек:Илим, 2010.

    Google Scholar

  • 加载中
通讯作者: 陈斌, bchen63@163.com
  • 1. 

    沈阳化工大学材料科学与工程学院 沈阳 110142

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索

Article Metrics

Article views(3559) PDF downloads(3285) Cited by(0)

Access History

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint