山东省大汶口盆地盐类矿床的地质成因探讨  

Stuty on the Origin of Salt Deposit in Dawenkou Basin in Shandong Province

作　　者：朱猛 

机构地区：[1]山东省鲁北地质工程勘查院,山东德州253015

出　　处：《山东国土资源》2015年第1期27-30,共4页Shandong Land and Resources

基　　金：山东省地质矿产勘查开发局资助项目(KY201304)

摘　　要：大汶口盆地是鲁西地区最大的一个沉积赋矿盆地,盆地内赋存丰富的矿产资源,岩盐矿、石膏矿、自然硫矿等,资源储量巨大。就大汶口盆地盐类矿床的形成条件问题,地质专家和学者一直有着不同的看法,该文从成矿物质来源、气候影响、古地理和地质构造因素等方面,对大汶口盆地矿床形成原因进行了探讨。Dwenkou basin is the biggest sedimentary ore -bearing basin in western Shandong province. Rich mineral resources occurred in this basin with abundant reserves, such as rock - salt deposit, gypsum deposit and native sulfur deposit. At present, geologistical experts and scholars hold different viewpoints on geological forming conditions of salt type deposits in Dawenkou basin. In this paper, from the aspects of minerals source, climate effects, paleogeography and geological structures, the forming origin of Dawenkou basin has been studied.

关 键 词：盐类矿床 沉积岩 地质成因 大汶口盆地 

分 类 号：P619.21[天文地球—矿床学]