Mineral Composition and Brittleness of Lower Cambrian Niutitang Formation Shale in Northwest Hunan

Zhen Zhang; Wen Pang; Linting Zhang; Peng Jiao; Xikai Wang

doi:10.18311/jmmf/2017/26968

Jump To References Section

Authors

Zhen Zhang
Key Laboratory of Metallogenic Prediction of Nonferrous Metals and Geological Environment Monitoring, Central South University, Ministry of Education, Central South University, Changsha 410 083 ,CN
Wen Pang
Shandong Shengli Vocational Institute of Training Department, Dongying 257000 ,CN
Linting Zhang
North China University of Science and Technology, Tangshan 063 210 ,CN
Peng Jiao
Key Laboratory of Metallogenic Prediction of Nonferrous Metals and Geological Environment Monitoring, Central South University, Ministry of Education, Central South University, Changsha 410 083 ,CN
Xikai Wang
Key Laboratory of Metallogenic Prediction of Nonferrous Metals and Geological Environment Monitoring, Central South University, Ministry of Education, Central South University, Changsha 410 083 ,CN

DOI:

https://doi.org/10.18311/jmmf/2017/26968

Keywords:

Shale, Components of Rock and Mineral, Brittleness, Niutitang Formation, Lower Cambrian, Northwest Hunan.

Abstract

This paper determines the mineral composition and analyzes the brittlenessof Lower Cambrian Niutitang formation shale in Northwest Hunan using XRD technology. The results show that Niutitang formation shale in Northwest Hunan has rather complicated composition, mainly consisting of quartz and clay minerals. The average content of quartz is 41.40%~60.81%, and the average content of clay minerals is 21.43%~26.40%. Calcite, plagioclase, dolomite, pyrite, potassium feldspar and other minerals are also commonly found in the samples. The brittle minerals of Niutitang formation shale are featured by rich species, high content (greater than 40% in average) and large brittleness index (higher than 50% in average). Compared to the shales in different regions both at home and abroad, Niutitang formation shale in Northwest Hunan has better fracability.