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滇南勐野井钾盐矿床成因新解
引用本文:欧天明.滇南勐野井钾盐矿床成因新解[J].云南地质,2014(1):6-13.
作者姓名:欧天明
作者单位:云南省地质矿产勘查开发局814队,云南昆明650400
摘    要:勐野井钾盐矿床的成因,众说纷纭.笔者将此矿床和兰坪思茅坳陷沉积盆地的演化与板块构造活动相结合,提出侏罗纪古钾盐矿经再溶蚀、再沉积、再改造的成因假说.认为今后在兰坪思茅坳陷探盐找钾的新方向是深埋在地下的中侏罗统和平乡组及下侏罗统,有可能在此层位找到大型或超大型的海相固体古钾盐矿床.

关 键 词:海相  侏罗系  古钾盐矿床  再改造  成因  云南滇南勐野井

A NEW RECOGNITION OF GENESIS OF MENGYEJING K SALT DEPOSIT IN S YUNNAN
OU Tian-ming.A NEW RECOGNITION OF GENESIS OF MENGYEJING K SALT DEPOSIT IN S YUNNAN[J].Yunnan Geology,2014(1):6-13.
Authors:OU Tian-ming
Affiliation:OU Tian-ming (C.eological Team 814, Yunnan Exploration & Development Bureau of Geology & Mineral Resources, Kunming 650400 )
Abstract:There are many opinions of the genesis of Mengyejing K salt deposit. We put forward the genesis hypothesis of resolution, re-sedimentation, re-reformation of Jurassic palaeo-k salt deposit, in combination of this ore deposit with the evolution of Simao depression sedimentation basin and plate tectonism. We think that the new direction of the future K and salt prospecting in Lanping-Simao depression is the deeply buried Middle Jurassic Hepingxiang Formation and Lower Jurassic, maybe the large or super-large scale marine solid palaeo-k salt deposit will be discovered in these horizons.
Keywords:Marine  Jurassic  Palaeo-K Salt Deposit  Re-reformation  Genesis  Mengyejing  S Yunnan
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