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Genesis and Prospecting Potential of the Da’anhe Skarn Au Deposit in the Central of the Lesser Xing’an Range, NE China: Evidence from Skarn Mineralogy, Fluid Inclusions and H-O Isotopes
Skarn Au deposits exist in the circum-pacific metallogenic belt. Interestingly, the Da’anhe Au deposit is the only independent skarn gold deposit in the Lesser Xing’an Range. To determine the metallogenic mechanism and prospecting potential of the Da’anhe deposit, we performed skarn mineralogy, flui...
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Published in: | Minerals (Basel) 2024-03, Vol.14 (3), p.214 |
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description | Skarn Au deposits exist in the circum-pacific metallogenic belt. Interestingly, the Da’anhe Au deposit is the only independent skarn gold deposit in the Lesser Xing’an Range. To determine the metallogenic mechanism and prospecting potential of the Da’anhe deposit, we performed skarn mineralogy, fluid inclusion (FI) and H-O isotope analyses. The results show the following: (1) The Da’anhe deposit is a calcareous reduced skarn Au deposit that formed between an Early Jurassic gabbroic diorite and the Permian Tumenling Formation marble. Its metallogenic process includes five stages: the early skarn stage (Stage I1), late skarn stage (Stage I2), early quartz-sulfide stage (Stage II1), late quartz-sulfide stage (Stage II2) and quartz-carbonate stage (Stage II3). Gold precipitated in Stage II1 and Stage II2. (2) The initial ore-forming fluid was derived from magmatic water and featured a high temperature and intermediate to high salinity. After boiling and mixing, the fluid eventually changed to a low-temperature and low-salinity reducing fluid dominated by meteoric water. (3) The formation depth of the Au orebodies was 2.27–3.11 km, and the orebodies were later lifted to the surface ( |
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Interestingly, the Da’anhe Au deposit is the only independent skarn gold deposit in the Lesser Xing’an Range. To determine the metallogenic mechanism and prospecting potential of the Da’anhe deposit, we performed skarn mineralogy, fluid inclusion (FI) and H-O isotope analyses. The results show the following: (1) The Da’anhe deposit is a calcareous reduced skarn Au deposit that formed between an Early Jurassic gabbroic diorite and the Permian Tumenling Formation marble. Its metallogenic process includes five stages: the early skarn stage (Stage I1), late skarn stage (Stage I2), early quartz-sulfide stage (Stage II1), late quartz-sulfide stage (Stage II2) and quartz-carbonate stage (Stage II3). Gold precipitated in Stage II1 and Stage II2. (2) The initial ore-forming fluid was derived from magmatic water and featured a high temperature and intermediate to high salinity. After boiling and mixing, the fluid eventually changed to a low-temperature and low-salinity reducing fluid dominated by meteoric water. (3) The formation depth of the Au orebodies was 2.27–3.11 km, and the orebodies were later lifted to the surface (<500 m). The potential for finding skarn Au deposits in the study area is limited. (4) The distinctive nature of the ore-related magma (i.e., source, reducing conditions and high water content) was key to the formation of the Da’anhe skarn gold deposit.</description><identifier>ISSN: 2075-163X</identifier><identifier>EISSN: 2075-163X</identifier><identifier>DOI: 10.3390/min14030214</identifier><language>eng</language><publisher>Basel: MDPI AG</publisher><subject>Anniversaries ; Carbonates ; Da’anhe Au deposit ; Diorite ; Exploration ; Fault lines ; fluid inclusion ; Fluid inclusions ; Geology ; Gold ; H-O isotopes ; High temperature ; Isotopes ; Jurassic ; Lava ; lesser Xing’an range ; Low temperature ; Magma ; Magmatic water ; Marble ; Metallogenesis ; Meteoric water ; Mineral deposits ; Mineralization ; Mineralogy ; Moisture content ; Molybdenum ; Permian ; Quartz ; Rocks ; Salinity ; Salinity effects ; skarn mineralogy ; Stone ; Stratigraphy ; Sulfides ; Sulphides ; Water content ; Water depth</subject><ispartof>Minerals (Basel), 2024-03, Vol.14 (3), p.214</ispartof><rights>COPYRIGHT 2024 MDPI AG</rights><rights>2024 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (https://creativecommons.org/licenses/by/4.0/). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-c361t-329b2189822cb6a050a69322f9f4ad88d58a46b5f15c50bf86ec839b64fdf0963</cites><orcidid>0000-0002-7148-8854</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.proquest.com/docview/3003356172/fulltextPDF?pq-origsite=primo$$EPDF$$P50$$Gproquest$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://www.proquest.com/docview/3003356172?pq-origsite=primo$$EHTML$$P50$$Gproquest$$Hfree_for_read</linktohtml><link.rule.ids>314,780,784,11688,25753,27924,27925,36060,37012,44363,44590,74895,75126</link.rule.ids></links><search><creatorcontrib>Zhao, Chuntao</creatorcontrib><creatorcontrib>Sun, Fanting</creatorcontrib><creatorcontrib>Sun, Jinggui</creatorcontrib><creatorcontrib>Wang, Jianping</creatorcontrib><creatorcontrib>Han, Jilong</creatorcontrib><creatorcontrib>Chu, Xiaolei</creatorcontrib><creatorcontrib>Bai, Chenglin</creatorcontrib><creatorcontrib>Yu, Dongmei</creatorcontrib><creatorcontrib>Xu, Zhikai</creatorcontrib><creatorcontrib>Yi, Lei</creatorcontrib><creatorcontrib>Hua, Shan</creatorcontrib><title>Genesis and Prospecting Potential of the Da’anhe Skarn Au Deposit in the Central of the Lesser Xing’an Range, NE China: Evidence from Skarn Mineralogy, Fluid Inclusions and H-O Isotopes</title><title>Minerals (Basel)</title><description>Skarn Au deposits exist in the circum-pacific metallogenic belt. Interestingly, the Da’anhe Au deposit is the only independent skarn gold deposit in the Lesser Xing’an Range. To determine the metallogenic mechanism and prospecting potential of the Da’anhe deposit, we performed skarn mineralogy, fluid inclusion (FI) and H-O isotope analyses. The results show the following: (1) The Da’anhe deposit is a calcareous reduced skarn Au deposit that formed between an Early Jurassic gabbroic diorite and the Permian Tumenling Formation marble. Its metallogenic process includes five stages: the early skarn stage (Stage I1), late skarn stage (Stage I2), early quartz-sulfide stage (Stage II1), late quartz-sulfide stage (Stage II2) and quartz-carbonate stage (Stage II3). Gold precipitated in Stage II1 and Stage II2. (2) The initial ore-forming fluid was derived from magmatic water and featured a high temperature and intermediate to high salinity. After boiling and mixing, the fluid eventually changed to a low-temperature and low-salinity reducing fluid dominated by meteoric water. (3) The formation depth of the Au orebodies was 2.27–3.11 km, and the orebodies were later lifted to the surface (<500 m). The potential for finding skarn Au deposits in the study area is limited. (4) The distinctive nature of the ore-related magma (i.e., source, reducing conditions and high water content) was key to the formation of the Da’anhe skarn gold deposit.</description><subject>Anniversaries</subject><subject>Carbonates</subject><subject>Da’anhe Au deposit</subject><subject>Diorite</subject><subject>Exploration</subject><subject>Fault lines</subject><subject>fluid inclusion</subject><subject>Fluid inclusions</subject><subject>Geology</subject><subject>Gold</subject><subject>H-O isotopes</subject><subject>High temperature</subject><subject>Isotopes</subject><subject>Jurassic</subject><subject>Lava</subject><subject>lesser Xing’an range</subject><subject>Low temperature</subject><subject>Magma</subject><subject>Magmatic water</subject><subject>Marble</subject><subject>Metallogenesis</subject><subject>Meteoric water</subject><subject>Mineral deposits</subject><subject>Mineralization</subject><subject>Mineralogy</subject><subject>Moisture content</subject><subject>Molybdenum</subject><subject>Permian</subject><subject>Quartz</subject><subject>Rocks</subject><subject>Salinity</subject><subject>Salinity effects</subject><subject>skarn mineralogy</subject><subject>Stone</subject><subject>Stratigraphy</subject><subject>Sulfides</subject><subject>Sulphides</subject><subject>Water content</subject><subject>Water 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and Prospecting Potential of the Da’anhe Skarn Au Deposit in the Central of the Lesser Xing’an Range, NE China: Evidence from Skarn Mineralogy, Fluid Inclusions and H-O Isotopes</title><author>Zhao, Chuntao ; Sun, Fanting ; Sun, Jinggui ; Wang, Jianping ; Han, Jilong ; Chu, Xiaolei ; Bai, Chenglin ; Yu, Dongmei ; Xu, Zhikai ; Yi, Lei ; Hua, Shan</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c361t-329b2189822cb6a050a69322f9f4ad88d58a46b5f15c50bf86ec839b64fdf0963</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2024</creationdate><topic>Anniversaries</topic><topic>Carbonates</topic><topic>Da’anhe Au deposit</topic><topic>Diorite</topic><topic>Exploration</topic><topic>Fault lines</topic><topic>fluid inclusion</topic><topic>Fluid inclusions</topic><topic>Geology</topic><topic>Gold</topic><topic>H-O isotopes</topic><topic>High 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(Basel)</jtitle><date>2024-03-01</date><risdate>2024</risdate><volume>14</volume><issue>3</issue><spage>214</spage><pages>214-</pages><issn>2075-163X</issn><eissn>2075-163X</eissn><abstract>Skarn Au deposits exist in the circum-pacific metallogenic belt. Interestingly, the Da’anhe Au deposit is the only independent skarn gold deposit in the Lesser Xing’an Range. To determine the metallogenic mechanism and prospecting potential of the Da’anhe deposit, we performed skarn mineralogy, fluid inclusion (FI) and H-O isotope analyses. The results show the following: (1) The Da’anhe deposit is a calcareous reduced skarn Au deposit that formed between an Early Jurassic gabbroic diorite and the Permian Tumenling Formation marble. Its metallogenic process includes five stages: the early skarn stage (Stage I1), late skarn stage (Stage I2), early quartz-sulfide stage (Stage II1), late quartz-sulfide stage (Stage II2) and quartz-carbonate stage (Stage II3). Gold precipitated in Stage II1 and Stage II2. (2) The initial ore-forming fluid was derived from magmatic water and featured a high temperature and intermediate to high salinity. After boiling and mixing, the fluid eventually changed to a low-temperature and low-salinity reducing fluid dominated by meteoric water. (3) The formation depth of the Au orebodies was 2.27–3.11 km, and the orebodies were later lifted to the surface (<500 m). The potential for finding skarn Au deposits in the study area is limited. (4) The distinctive nature of the ore-related magma (i.e., source, reducing conditions and high water content) was key to the formation of the Da’anhe skarn gold deposit.</abstract><cop>Basel</cop><pub>MDPI AG</pub><doi>10.3390/min14030214</doi><orcidid>https://orcid.org/0000-0002-7148-8854</orcidid><oa>free_for_read</oa></addata></record> |
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subjects | Anniversaries Carbonates Da’anhe Au deposit Diorite Exploration Fault lines fluid inclusion Fluid inclusions Geology Gold H-O isotopes High temperature Isotopes Jurassic Lava lesser Xing’an range Low temperature Magma Magmatic water Marble Metallogenesis Meteoric water Mineral deposits Mineralization Mineralogy Moisture content Molybdenum Permian Quartz Rocks Salinity Salinity effects skarn mineralogy Stone Stratigraphy Sulfides Sulphides Water content Water depth |
title | Genesis and Prospecting Potential of the Da’anhe Skarn Au Deposit in the Central of the Lesser Xing’an Range, NE China: Evidence from Skarn Mineralogy, Fluid Inclusions and H-O Isotopes |
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