摘要
探讨非传统方法在塔里木盆地寻找钾盐,尝试通过古盐度计算和古地理恢复来确定潟湖相沉积中心,同时结合元素地球化学特征分析与古地理、古盐度的耦合关系,对塔里木盆地固体钾盐矿有利发育区进行预测,认为发育深水潟湖相的大宛其地区岩盐体最厚,古盐度值、K+含量和溴氯系数也最高,并从深水潟湖→浅水潟湖→潟湖边缘呈逐渐递减趋势。大宛其地区具有优越的成钾条件,应为塔里木盆地固体钾盐矿勘查优选目标。
Tarim Basin is one of the most important and alive ancient potash mine exploration areas.In the past researches,the studies mainly focused attention on the characteristics of element geochemistry,and the traditional methods were difficult to find potassium.This article tries to define the depocenter of lagoon facies halite by palaeosalinity calculation and palaeogeographic reconstruction.Combined with the coupling relationship of element geochemistry characteristics,palaeogeography,and palaeosalinity,the author predicts the beneficial area for ancient potash mine and considers the Dawanqi area where deep-water lagoon facies develop has the thickest halite,highest palaeosalinity,K＋ content,and coefficient of Br and Cl.All of these present a decline trend from deep-water lagoon,shallow lagoon to the edge of lagoon.According to multidisciplinary analysis,the author considers that the Dawanqi area in Kuche Basin has superior forming-potassium conditions,and it should be the optimum exploration target of ancient potash mines in Tarim Basin.
出处
《成都理工大学学报（自然科学版）》
CAS
CSCD
北大核心
2011年第2期185-190,共6页
Journal of Chengdu University of Technology: Science & Technology Edition
基金
国家青年科学基金项目(41002033)
国家科技重大专项(2008ZX05030-003-02)
关键词
塔里木盆地
钾盐
古盐度
古地理
地球化学特征
Tarim Basin
potash salt
palaeosalinity
palaeogeography
geochemical characters
