天青石矿床

四川合川天青石矿床位于合川县盐井镇之西2km处。

Hechuan celestine deposit of Sichuan is situated in 2 km west of Yanjing village in Hechuan county .

从锶的地球化学特征探讨天青石矿床的成因类型及找矿方向

Genetic types of celestite deposits and their prospecting direction discussed from strontium geochemistry

合川天青石矿床成矿地球化学及形成机理

The Mineralization Geochemistry and Formation Mechanism of Hechuan Celestine

认为本矿床应届沉积&改造类型的天青石矿床。

Therefore , the author considers the deposit to be a sedimentary-transform type of celestine .

四川会理拉拉铜矿地球化学特征及其大陆动力学背景合川天青石矿床成矿地球化学及形成机理

The Geochemical Characteristics and Continental Geodynamics of Lala Copper Deposit ; The Mineralization Geochemistry and Formation Mechanism of Hechuan Celestine

重庆地区天青石型锶矿床成矿特征

Metallogenic characteristics of the celestite type SR deposit in Chongqing area

中国（天青石）锶矿床概述

Celestite ( SR ) deposits in China

依据成矿作用和成矿地质特征，将我国（天青石）锶矿床划分为沉积型、岩浆热液型、沉积热卤水改造型和表生淋积型等四大类七个亚类。

According to mineralizing conditions and processes , the deposits may be grouped into sedimentary , hydrothermal , sediment reworked and supergene leaching , including four types and seven subtypes .

天青石矿是后生矿床，其成矿物质主要来自三叠纪含盐系。

The celestite ore was epigenetic , its mineralization substances mostly came from the Triassic salty series .