世界地质    2017 36 (3): 954-963   ISSN: 1004-5589  CN: 22-1111/P   火山岩磁化率特征及其影响因素：以准东石炭系巴塔玛依内山组为例 陈宪1, 边伟华1, 王林涛1, 杨凯凯1, 张增宝2, 李昭3 1. 吉林大学地球科学学院, 长春 130061; 2. 中石化胜利油田分公司油气勘探管理中心, 山东东营 257000; 3. 中国地质调查局油气资源调查中心, 北京 100029 收稿日期 2017-03-01  修回日期 2017-04-01  网络版发布日期 null 参考文献  [1] Dunlop D J, Özdemir Ö. Rock magnetism:fundamentals and frontiers[M]. Cambridge(UK):Cambridge University Press, 1997:24-34. [2] 张拴宏,周显强.磁化率各向异性地学应用综述[J].地质论评,1999, 45(6):613-620. ZHANG Shuang-hong, ZHOU Xian-qiang. A review of the application of anisotropy of susceptibility to Earth Science[J]. Geological Review, 1999, 45(6):613-620. [3] 王建,刘泽纯,姜文英,等.磁化率与粒度、矿物的关系及其古环境意义[J].地理学报,1996, 51(2):155-163. WANG Jian, LIU Ze-chun, JIANG Wen-ying, et al. A relationship between susceptibility and grain-size and minerals, and their paleo-environment implications[J]. Acta Geographica Sinica, 1996, 51(2):155-163. [4] 徐新文,强小科,安芷生,等.鹤庆盆地湖相岩心磁化率记录及其古环境意义[J].地质力学学报, 2010, 16(4):372-382. 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