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Porphyry Copper Deposit Prognosis in the Middle Region of the Bangonghu–Nujiang Metallogenic Belt, Tibet, Using ASTER Remote Sensing Data

The Bangonghu–Nujiang metallogenic belt is considered to be Tibet’s third copper belt after the Yulong and Gangdese copper belts. The Duolong gold‐rich porphyry copper deposit, located in the western part of the Bangonghu–Nujiang belt was recently recognized as a superlarge prospect. The Advanced Sp...

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Published in:Resource geology 2018-01, Vol.68 (1), p.65-82
Main Authors: Dai, Jingjing, Qu, Xiaoming, Song, Yang
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description The Bangonghu–Nujiang metallogenic belt is considered to be Tibet’s third copper belt after the Yulong and Gangdese copper belts. The Duolong gold‐rich porphyry copper deposit, located in the western part of the Bangonghu–Nujiang belt was recently recognized as a superlarge prospect. The Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) was used to characterize the Duolong porphyry deposit alteration area, and three methods, color enhancement, band ratio transformation, and spectral angle mapping, were utilized to extract the phyllic and argillic alteration zones, which are typically considered the most important predictors of porphyry copper. Seven prospecting areas, which match mapped alteration zones, were delineated in the Duolong deposit. In addition, an ASTER image of the eastern region of the Bangonghu–Nujiang belt in the Xiongmei area was used to extract alteration information, and an area with image characteristics similar to the Duobuza and Bolong ore deposits was identified as a prospecting area. Numerous malachite outcrops were identified in the field, and both laboratory analysis and isotopic dating confirmed that the deposit had formed concurrently with the Duobuza deposit (119 Ma). Geologic mapping at the 1:5000 scale was conducted in the area, and three types of ore‐bearing rocks were identified, indicating that this area has significant potential to host ore deposits. The discovery of the Xiongmei copper mining area is significant for the Bangonghu–Nujiang belt. ASTER remote sensing data are used to study the Duolong porphyry copper deposit and Bangearea in Tibet. Color enhancement, band ratio transformation, and spectral angle mapping are applied. Based on these three methods, hydrothermal alteration zones are extracted, and the Xiongmei area in Bange is conformed to be a potential copper mining deposit from geological and geochemical evidence.
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Numerous malachite outcrops were identified in the field, and both laboratory analysis and isotopic dating confirmed that the deposit had formed concurrently with the Duobuza deposit (119 Ma). Geologic mapping at the 1:5000 scale was conducted in the area, and three types of ore‐bearing rocks were identified, indicating that this area has significant potential to host ore deposits. The discovery of the Xiongmei copper mining area is significant for the Bangonghu–Nujiang belt. ASTER remote sensing data are used to study the Duolong porphyry copper deposit and Bangearea in Tibet. Color enhancement, band ratio transformation, and spectral angle mapping are applied. 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Numerous malachite outcrops were identified in the field, and both laboratory analysis and isotopic dating confirmed that the deposit had formed concurrently with the Duobuza deposit (119 Ma). Geologic mapping at the 1:5000 scale was conducted in the area, and three types of ore‐bearing rocks were identified, indicating that this area has significant potential to host ore deposits. The discovery of the Xiongmei copper mining area is significant for the Bangonghu–Nujiang belt. ASTER remote sensing data are used to study the Duolong porphyry copper deposit and Bangearea in Tibet. Color enhancement, band ratio transformation, and spectral angle mapping are applied. 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Numerous malachite outcrops were identified in the field, and both laboratory analysis and isotopic dating confirmed that the deposit had formed concurrently with the Duobuza deposit (119 Ma). Geologic mapping at the 1:5000 scale was conducted in the area, and three types of ore‐bearing rocks were identified, indicating that this area has significant potential to host ore deposits. The discovery of the Xiongmei copper mining area is significant for the Bangonghu–Nujiang belt. ASTER remote sensing data are used to study the Duolong porphyry copper deposit and Bangearea in Tibet. Color enhancement, band ratio transformation, and spectral angle mapping are applied. 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subjects alteration information extraction
Area
ASTER (radiometer)
Bangonghu–Nujiang metallogenic belt
Colour
Copper
Copper ores
Dating techniques
Exploration
Geologic mapping
Geological mapping
Gold
Identification
Information processing
Mapping
Mineral deposits
Mining
ore prediction
Outcrops
Porphyry copper
porphyry copper deposit
Radiometers
Remote sensing
Thermal emission
Transformations (mathematics)
title Porphyry Copper Deposit Prognosis in the Middle Region of the Bangonghu–Nujiang Metallogenic Belt, Tibet, Using ASTER Remote Sensing Data
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