FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4384202208> ?p ?o ?g. }

• W4384202208 endingPage "8118" @default.
• W4384202208 startingPage "8118" @default.
• W4384202208 abstract "Studying the activation, migration and precipitation processes of ore-forming elements is essential for understanding the genesis and mechanisms of skarn deposits. A typical skarn profile formed by the intrusion of Yanshanian granodiorite into the Carboniferous carbonate strata was studied. The profile is highly consistent with the classic skarn profile, ranging from the intrusion, weak alteration belt, skarn belt (inner and outer skarn belt) and mineralization belt (mainly characterized by Cu mineralization) to the surrounding marble without being affected by late-stage low-temperature or supergene weathering alteration. Whole-rock data show that the major and trace elements exhibit relatively small changes in the granodiorite and inner skarn, but huge variation in the boundary between the inner and outer skarn; Na, Al, Ti and Sr show significant decreases, while Fe, Mg, Zn, V and Ni show significant increases. The elemental content in the outer skarn is 10–100 times or more higher than that in the marble, but the elements such as Ca, Sr and Cs diluted from the marble. During the migration process from the inner skarn to the outer skarn, some elements (such as K, Rb and Ba) were depleted in the inner, but not enriched in the outer, indicating that they may migrate to farther locations. Grossularite developed in the inner skarn, with light rare earth element (LREE) depletion and heavy REE enrichment, as well as positive and negative anomalies of Eu (δEu = 0.42–3.95). Andradite developed in the outer skarn, with zonation development, light REE enrichment, and heavy REE depletion and a positive Eu anomaly (δEu = 0.36–46.83). Some negative Eu anomalies appear at the edges of garnets in the outer skarn, indicating fluctuations in fO2 during the late skarn process. A positive correlation between Fe3+ and REE3+ in the garnets from the inner skarn, as well as between Al3+ and REE3+ from the outer skarn indicated that there are different YAG substitution mechanisms of REE between the inner and outer skarn. Low garnet REE contents and highly variable Y/Ho ratios in outer skarn suggest that the significant fluctuations in REEs may be primarily controlled by water-rock interactions. Considering the whole-rock major and trace element contents, as well as the trace element features of garnet, we found that whole-rock Na, Al, Ti and Sr elements, garnet Ti, Zr and Nb elements exhibit significant differences between the inner and outer skarn. These characteristics can be used to distinguish the boundary between the rock body and carbonate during the skarnification process." @default.
• W4384202208 created "2023-07-14" @default.
• W4384202208 creator A5052716256 @default.
• W4384202208 creator A5080605980 @default.
• W4384202208 creator A5087650455 @default.
• W4384202208 date "2023-07-12" @default.
• W4384202208 modified "2023-09-29" @default.
• W4384202208 title "Whole Rock, Mineral Chemistry during Skarn Mineralization-Case Study from Tongshan Cu-Mo Skarn Profile" @default.
• W4384202208 cites W1964432997 @default.
• W4384202208 cites W1974235181 @default.
• W4384202208 cites W1982560803 @default.
• W4384202208 cites W1990367391 @default.
• W4384202208 cites W2001119618 @default.
• W4384202208 cites W2008632542 @default.
• W4384202208 cites W2011562340 @default.
• W4384202208 cites W2013438296 @default.
• W4384202208 cites W2013447206 @default.
• W4384202208 cites W2017637482 @default.
• W4384202208 cites W2032851167 @default.
• W4384202208 cites W2037429669 @default.
• W4384202208 cites W2051805987 @default.
• W4384202208 cites W2052064329 @default.
• W4384202208 cites W2056734066 @default.
• W4384202208 cites W2064369753 @default.
• W4384202208 cites W2067273506 @default.
• W4384202208 cites W2072618050 @default.
• W4384202208 cites W2076382171 @default.
• W4384202208 cites W2084239657 @default.
• W4384202208 cites W2092235118 @default.
• W4384202208 cites W2105875032 @default.
• W4384202208 cites W2126978098 @default.
• W4384202208 cites W2133042542 @default.
• W4384202208 cites W2135214884 @default.
• W4384202208 cites W2140093647 @default.
• W4384202208 cites W2152195282 @default.
• W4384202208 cites W2154416358 @default.
• W4384202208 cites W2159947526 @default.
• W4384202208 cites W2167590372 @default.
• W4384202208 cites W2329970122 @default.
• W4384202208 cites W2396410649 @default.
• W4384202208 cites W2789226214 @default.
• W4384202208 cites W2886463320 @default.
• W4384202208 cites W2975922265 @default.
• W4384202208 cites W2996418589 @default.
• W4384202208 cites W3155600757 @default.
• W4384202208 cites W3201832421 @default.
• W4384202208 cites W4220776069 @default.
• W4384202208 cites W4220990979 @default.
• W4384202208 cites W4306692474 @default.
• W4384202208 cites W4366371562 @default.
• W4384202208 doi "https://doi.org/10.3390/app13148118" @default.
• W4384202208 hasPublicationYear "2023" @default.
• W4384202208 type Work @default.
• W4384202208 citedByCount "0" @default.
• W4384202208 crossrefType "journal-article" @default.
• W4384202208 hasAuthorship W4384202208A5052716256 @default.
• W4384202208 hasAuthorship W4384202208A5080605980 @default.
• W4384202208 hasAuthorship W4384202208A5087650455 @default.
• W4384202208 hasBestOaLocation W43842022081 @default.
• W4384202208 hasConcept C111696902 @default.
• W4384202208 hasConcept C127313418 @default.
• W4384202208 hasConcept C151730666 @default.
• W4384202208 hasConcept C156622251 @default.
• W4384202208 hasConcept C159390177 @default.
• W4384202208 hasConcept C159750122 @default.
• W4384202208 hasConcept C167919410 @default.
• W4384202208 hasConcept C17409809 @default.
• W4384202208 hasConcept C178790620 @default.
• W4384202208 hasConcept C185592680 @default.
• W4384202208 hasConcept C195843664 @default.
• W4384202208 hasConcept C199289684 @default.
• W4384202208 hasConcept C2776152364 @default.
• W4384202208 hasConcept C2776989079 @default.
• W4384202208 hasConcept C2778188036 @default.
• W4384202208 hasConcept C2779712906 @default.
• W4384202208 hasConcept C544778455 @default.
• W4384202208 hasConcept C67236022 @default.
• W4384202208 hasConcept C7145564 @default.
• W4384202208 hasConceptScore W4384202208C111696902 @default.
• W4384202208 hasConceptScore W4384202208C127313418 @default.
• W4384202208 hasConceptScore W4384202208C151730666 @default.
• W4384202208 hasConceptScore W4384202208C156622251 @default.
• W4384202208 hasConceptScore W4384202208C159390177 @default.
• W4384202208 hasConceptScore W4384202208C159750122 @default.
• W4384202208 hasConceptScore W4384202208C167919410 @default.
• W4384202208 hasConceptScore W4384202208C17409809 @default.
• W4384202208 hasConceptScore W4384202208C178790620 @default.
• W4384202208 hasConceptScore W4384202208C185592680 @default.
• W4384202208 hasConceptScore W4384202208C195843664 @default.
• W4384202208 hasConceptScore W4384202208C199289684 @default.
• W4384202208 hasConceptScore W4384202208C2776152364 @default.
• W4384202208 hasConceptScore W4384202208C2776989079 @default.
• W4384202208 hasConceptScore W4384202208C2778188036 @default.
• W4384202208 hasConceptScore W4384202208C2779712906 @default.
• W4384202208 hasConceptScore W4384202208C544778455 @default.
• W4384202208 hasConceptScore W4384202208C67236022 @default.
• W4384202208 hasConceptScore W4384202208C7145564 @default.
• W4384202208 hasIssue "14" @default.

• next