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老挝万象地区含盐系地层
引用本文:冯明刚,吴军,韩润生,朱延浙,严城民.老挝万象地区含盐系地层[J].云南地质,2005,24(4):407-413.
作者姓名:冯明刚  吴军  韩润生  朱延浙  严城民
作者单位:1. 昆明理工大学国土资源工程学院,昆明,650093
2. 云南地矿勘查工程总公司,老挝钾盐项目经理部,昆明,650216
基金项目:中国地质调查局,老挝万象平原钾镁盐矿勘查。
摘    要:老挝万象地区的含盐地层称为塔贡组(E1tg)。该组可划分为三个岩性段,每个岩性段均由下部膏盐层、上部陆源碎屑岩组成,均属湖泊沉积。该套地层的介形虫属Sinocypris—Cypris(Cristocypris)—Parailyocypris组合、轮藻属Peckichara—Obtusochara组合,属古新统。岩石地层、生物地层及年代地层上,该组与我国滇西地区的勐野井组(Em)较为相似。

关 键 词:含盐地层  剖面与岩性  地层时代  万象平原老挝
文章编号:1004-1885(2005)04-407-07
收稿时间:2005-06-13
修稿时间:2005-06-13

THE SALT-BEARING STRATA IN VIENTIANE PLAIN, LAOS
FENG Ming-gang,WU Jun,HAN Run-sheng,ZHU Yan-zhe,YAN Cheng-min.THE SALT-BEARING STRATA IN VIENTIANE PLAIN, LAOS[J].Yunnan Geology,2005,24(4):407-413.
Authors:FENG Ming-gang  WU Jun  HAN Run-sheng  ZHU Yan-zhe  YAN Cheng-min
Abstract:The salt-bearing strata in Vientiane area, Laos are called Thangon Formation(E_1tg), which can be divided into 3 lithological members. And every lithological member is composed of the lower gypsiferous salt bed and the upper terrigenous clastic rock, which belongs to the lacustrine sediment. The geological period of Sinocypris-Cypris(Cristocypris)-Parailyocypris Ostracoda assemblage and Peckichara-Obtuschara Charophyta assemblage belongs to Palaeocene. In lithology, stratigraphy, biostratigra- phy and chronostratigraphy, Thangon Formation is relatively similar to Mengyejing Formation(E_1m) in the area of West Yunnan, China.
Keywords:Salt-Bearing Strata  Lithostratigraphy  Biostratigraphy  Chronostratigraphy  Vientiane Area  Laos
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