Chromite-Bearing Peridotite Identification, Based on Spectral Analysis and Machine Learning: A Case Study of the Luobusa Area, Tibet, China

Author:

Yang Weiguang123,Zheng Youye24ORCID,Chen Shizhong135,Duan Xingxing13,Zhou Yu13,Xu Xiaokuan6

Affiliation:

1. Urumqi Comprehensive Survey Center on Natural Resources, China Geological Survey, Urumqi 830057, China

2. School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China

3. Innovation Base of Metallogenic Prediction and Prospecting in Central Asia Orogenic Belt, Chinese Geological Society, Urumqi 830057, China

4. Institute of Geological Survey, China University of Geosciences, Wuhan 430074, China

5. Nanjing Geological Survey Center, China Geological Survey, Nanjing 210016, China

6. Faculty of Science and Technology, University of Canberra, Canberra 2601, Australia

Abstract

Chromite is a strategic mineral resource for many countries, and chromite deposit occurrences are widespread in the ultramafic rocks of the Yarlung Zangbo ophiolite belt, particularly in the harzburgite unit of the mantle section. Conducting field surveys in complex and poorly accessible terrain is challenging, expensive, and time-consuming. Remote sensing is an advanced method of achieving modern geological work and is a powerful technical means of geological research and mineral exploration. In order to delineate outcrops of chromite-bearing mantle peridotite, the present research study integrates seven image-enhancement techniques, including optimal band combination, decorrelation stretching, band ratio, independent component analysis, principal component analysis, minimum noise fraction, and false color composite, for the interpretation of Landsat8 OLI and WorldView-2 satellite data. This integrated approach allows the effective discrimination of chromite-containing peridotite outcrops in the Luobusa area, Tibet. The interpretation results derived from these integrated image-processing techniques were systematically verified in the field and formed the basis of the feature selection process of different lithologies supported by the support vector machine algorithm. Furthermore, the distribution range of the ferric contamination anomaly is detected through the de-interference abnormal principal component thresholding technique, which shows a high spatial matching relationship with mantle peridotite. This is the first study to utilize Landsat8 OLI and WorldView-2 remote sensing satellite data to explore the largest chromite deposit in China, which enriches the research methods for the chromite deposits in the Luobusa area. Accordingly, the results of this investigation indicate that the integration of information extracted from image-processing algorithms using remote sensing data could be a broadly applicable tool for prospecting chromite ore deposits associated with ophiolitic complexes in mountainous and inaccessible regions such as Tibet’s ophiolitic zones.

Funder

Secondary Project of China Geological Survey

Natural Science Foundation of Xinjiang Uygur Autonomous Region

Publisher

MDPI AG

Subject

Fluid Flow and Transfer Processes,Computer Science Applications,Process Chemistry and Technology,General Engineering,Instrumentation,General Materials Science

Reference110 articles.

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2. Some opinions on further exploration for chromite deposits in the Luobusha area, Tibet, China;Wang;Geol. Bull. China,2010

3. Application of ASTER and Landsat TM Data for Geological Mapping of Esfandagheh Ophiolite Complex, Southern Iran;Pournamdari;Resour. Geol.,2014

4. High-Cr and high-Al chromitite found in western Yar-lung-Zangbo suture zone in Tibet;Xiong;Acta Petrol. Sin.,2013

5. Chromitites in ophiolites: Questions and thoughts;Yang;Acta Geol. Sin.,2022

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