Pb-Zn Deposits and Associated Critical Metals
As base metals, zinc and lead are widely developed in various types of deposits. Zinc and lead also form various types of independent deposits and are associated with a variety of critical metals. Zn-Pb deposits occupy an important position in the world, including volcanic-hosted massive sulphide (V...
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| Format: | Electronic Book Chapter |
| Language: | English |
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MDPI - Multidisciplinary Digital Publishing Institute
2023
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| Online Access: | DOAB: download the publication DOAB: description of the publication |
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| 072 | 7 | |a R |2 bicssc | |
| 100 | 1 | |a Zhou, Jia-Xi |4 edt | |
| 700 | 1 | |a Zhang, Changqing |4 edt | |
| 700 | 1 | |a Ren, Tao |4 edt | |
| 700 | 1 | |a Wu, Yue |4 edt | |
| 700 | 1 | |a Zhou, Jia-Xi |4 oth | |
| 700 | 1 | |a Zhang, Changqing |4 oth | |
| 700 | 1 | |a Ren, Tao |4 oth | |
| 700 | 1 | |a Wu, Yue |4 oth | |
| 245 | 1 | 0 | |a Pb-Zn Deposits and Associated Critical Metals |
| 260 | |b MDPI - Multidisciplinary Digital Publishing Institute |c 2023 | ||
| 300 | |a 1 electronic resource (244 p.) | ||
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| 506 | 0 | |a Open Access |2 star |f Unrestricted online access | |
| 520 | |a As base metals, zinc and lead are widely developed in various types of deposits. Zinc and lead also form various types of independent deposits and are associated with a variety of critical metals. Zn-Pb deposits occupy an important position in the world, including volcanic-hosted massive sulphide (VHMS/VMS), magmatic-hydrothermal-associated skarn and/or epithermal types, sediment-hosted types (e.g., clastic-hosted sedimentary exhalative, SEDEX; carbonate-hosted Mississippi Valley type, MVT; sandstone-hosted type, SST; and shale-hosted type), and hydrothermal vein types. This Special Issue reprint aims to provide a comprehensive understanding of Zn-Pb deposits and associated critical metals, and promote global prospecting. | ||
| 540 | |a Creative Commons |f https://creativecommons.org/licenses/by/4.0/ |2 cc |4 https://creativecommons.org/licenses/by/4.0/ | ||
| 546 | |a English | ||
| 650 | 7 | |a Research & information: general |2 bicssc | |
| 650 | 7 | |a Earth sciences, geography, environment, planning |2 bicssc | |
| 653 | |a machine learning | ||
| 653 | |a sphalerite | ||
| 653 | |a LA-ICP-MS | ||
| 653 | |a Pb-Zn deposits | ||
| 653 | |a web app | ||
| 653 | |a fault structure | ||
| 653 | |a dispersed metals | ||
| 653 | |a fractal structure characteristic | ||
| 653 | |a Fry analysis | ||
| 653 | |a prospecting direction | ||
| 653 | |a eastern Guizhou metallogenic belt | ||
| 653 | |a SW China | ||
| 653 | |a 3D deposit model | ||
| 653 | |a weight of evidence method | ||
| 653 | |a neural network method | ||
| 653 | |a metallogenic prediction | ||
| 653 | |a the Dulong Sn-Zn polymetallic deposit | ||
| 653 | |a Sichuan-Yunnan-Guizhou Pb-Zn metallogenic province | ||
| 653 | |a Lekai Pb-Zn deposit | ||
| 653 | |a calcite/dolomite REE | ||
| 653 | |a C-O-Mg isotope | ||
| 653 | |a metallogenic fluid source | ||
| 653 | |a in situ S and Pb isotopes | ||
| 653 | |a the source of ore-forming elements | ||
| 653 | |a ore genesis | ||
| 653 | |a Caiyuanzi Pb-Zn deposit | ||
| 653 | |a porosity | ||
| 653 | |a permeability | ||
| 653 | |a lead-zinc ore | ||
| 653 | |a Huize | ||
| 653 | |a altered wall rocks | ||
| 653 | |a in situ S isotope | ||
| 653 | |a elemental geochemistry | ||
| 653 | |a pyrite | ||
| 653 | |a Fule Pb-Zn deposit | ||
| 653 | |a northeast Yunnan | ||
| 653 | |a China | ||
| 653 | |a Banbianjie Ge-Zn deposit | ||
| 653 | |a gangue minerals | ||
| 653 | |a nature | ||
| 653 | |a source and evolution of ore-forming fluids | ||
| 653 | |a trace elements | ||
| 653 | |a Western Hunan-Eastern Guizhou Pb-Zn metallogenic belt | ||
| 653 | |a garnet | ||
| 653 | |a granite porphyry | ||
| 653 | |a ore-forming age | ||
| 653 | |a tectonic setting | ||
| 653 | |a in-site trace elements | ||
| 653 | |a substitution mechanisms | ||
| 653 | |a Nanmushu Zn-Pb deposit | ||
| 653 | |a Mayuan district | ||
| 653 | |a Mississippi Valley-type (MVT) deposit | ||
| 653 | |a smithsonite | ||
| 653 | |a ore deposit genesis | ||
| 653 | |a supergene oxidation | ||
| 653 | |a Huoshaoyun deposit | ||
| 653 | |a resistivity | ||
| 653 | |a chargeability | ||
| 653 | |a mineral exploration | ||
| 653 | |a 2D and 3D inversion | ||
| 856 | 4 | 0 | |a www.oapen.org |u https://mdpi.com/books/pdfview/book/7795 |7 0 |z DOAB: download the publication |
| 856 | 4 | 0 | |a www.oapen.org |u https://directory.doabooks.org/handle/20.500.12854/113951 |7 0 |z DOAB: description of the publication |