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Siliceous-sulphate rock coatings at Zhenzhu Spring, Tengchong, China: the integrated product of acid-fog deposition, spring water capillary action, and dissolution

Published online by Cambridge University Press:  06 June 2019

Huaguo Wen Open the ORCID record for Huaguo Wen [Opens in a new window] ,
Wenli Xu ,
Yi Li ,
Yaxian You  and
Xiaotong Luo
Huaguo Wen*
Affiliation:
State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 610059, China Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, China
Wenli Xu*
Affiliation:
State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 610059, China Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, China
Yi Li
Affiliation:
Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, China
Yaxian You
Affiliation:
Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, China
Xiaotong Luo
Affiliation:
Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, China
*
Author for correspondence: Huaguo Wen and Wenli Xu, Emails: wenhuaguo08@cdut.cn; xuwenli5@163.com
Author for correspondence: Huaguo Wen and Wenli Xu, Emails: wenhuaguo08@cdut.cn; xuwenli5@163.com
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Abstract

Siliceous-sulphate rock coatings were observed at Zhenzhu Spring, an acid sulphate hot spring in the Tengchong volcanic field, China. These rock coatings are mainly formed of gypsum and amorphous silica. Some alum-(K), voltaite, α-quartz and muscovite were also found. Four different laminae are developed in the rock coatings: gypsum layer, tight siliceous layer, tabular siliceous layer and siliceous debris layer. The gypsum layer is located at the top of the rock coatings, while other siliceous layers appear below the gypsum layer. Geochemical modelling of the fluids was performed to identify the mechanisms responsible for the formation of gypsum and amorphous silica. The results indicated that the occurrence of gypsum is related to the acid-fog deposition and amorphous silica mainly originates from spring water. Fog deposition provided the rock coatings with abundant SO42− and Ca, and the subsequent complete evaporation of the condensed fluids produced gypsum. Seasonal climate change (especially variation in rainfall) determines the fluctuations of capillary action and dissolution. Rainfall events in the wet season led to periods of non-precipitating gypsum and promoted the capillary rise of the spring water. Slightly diluted capillary water (a small amount of rainwater) covered the rock coatings, formed a tight siliceous layer on the rock-coating surface and/or filled the pores among the gypsum crystals forming many tabular siliceous aggregates. Heavy rainfall (high dilution), however, resulted in non-precipitating amorphous silica and accelerated the gypsum dissolution, leaving tabular pores around tabular siliceous aggregates and forming a tabular siliceous layer.

Keywords

gypsumamorphous silicarock coatinghot springTengchong
Type
Original Article
Information
Geological Magazine , Volume 157 , Issue 2 , February 2020 , pp. 201 - 212
Copyright
© Cambridge University Press 2019 

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