Mineral Chemistry of Low-Temperature Phyllosilicates in Early Paleozoic Metaclastic Rocks, Eastern Tauride Belt, Türkiye
The mineral chemistry of illite/mica and chlorites, together with the evaluation of textural data of low-temperature metaclastic rocks, plays an important role in determining their origin and metamorphic grade. This study aimed to investigate the chemical properties of phyllosilicates in early Paleo...
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| Veröffentlicht in: | Minerals (Basel) 2022-09, Vol.12 (9), p.1088 |
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| description | The mineral chemistry of illite/mica and chlorites, together with the evaluation of textural data of low-temperature metaclastic rocks, plays an important role in determining their origin and metamorphic grade. This study aimed to investigate the chemical properties of phyllosilicates in early Paleozoic metaclastic rocks in the Eastern Tauride Belt, Türkiye. The textural (electron microscopy) and chemical (mineral chemistry analysis) analyses were performed on the samples representing different grades of metamorphism. The illites/micas and chlorites are observed as detrital (chlorite–mica stacks) and neoformation origin. Trioctahedral chlorites (chamosite) exhibit different chemistry for detrital and neoformed origin as well as the metamorphic grade. Tetrahedral Al and octahedral Fe + Mg increase, whereas octahedral Al decreases together with the increasing grade of metamorphism. The detrital chlorites have higher tetrahedral Al and Fe contents than their neoformed counterparts. Chlorite geothermometry data (detrital: 241–≥350 °C; neoformed: 201–268 °C) are compatible with the texture and illite Kübler index data. Illite/white-mica compositions display muscovite and Na-K mica. Tetrahedral Al and interlayer K + Na contents of illites/micas increase with metamorphic grade. Na-K mica and paragonite are observed as replacement-type developments within the detrital CMS. The obtained data indicate that phyllosilicate chemistry can be used effectively for determining the geological evolution of low-grade metamorphic sequences. |
| doi_str_mv | 10.3390/min12091088 |
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This study aimed to investigate the chemical properties of phyllosilicates in early Paleozoic metaclastic rocks in the Eastern Tauride Belt, Türkiye. The textural (electron microscopy) and chemical (mineral chemistry analysis) analyses were performed on the samples representing different grades of metamorphism. The illites/micas and chlorites are observed as detrital (chlorite–mica stacks) and neoformation origin. Trioctahedral chlorites (chamosite) exhibit different chemistry for detrital and neoformed origin as well as the metamorphic grade. Tetrahedral Al and octahedral Fe + Mg increase, whereas octahedral Al decreases together with the increasing grade of metamorphism. The detrital chlorites have higher tetrahedral Al and Fe contents than their neoformed counterparts. Chlorite geothermometry data (detrital: 241–≥350 °C; neoformed: 201–268 °C) are compatible with the texture and illite Kübler index data. Illite/white-mica compositions display muscovite and Na-K mica. Tetrahedral Al and interlayer K + Na contents of illites/micas increase with metamorphic grade. Na-K mica and paragonite are observed as replacement-type developments within the detrital CMS. The obtained data indicate that phyllosilicate chemistry can be used effectively for determining the geological evolution of low-grade metamorphic sequences.</description><identifier>ISSN: 2075-163X</identifier><identifier>EISSN: 2075-163X</identifier><identifier>DOI: 10.3390/min12091088</identifier><language>eng</language><publisher>Basel: MDPI AG</publisher><subject>Aluminum ; Belts ; Carbon ; Chemical properties ; Chemicophysical properties ; Chemistry ; Chlorite ; Chlorites ; Electron microscopy ; Illite ; Illites ; Interlayers ; Investigations ; Iron ; Laboratories ; Low temperature ; Magnesium ; Metamorphism ; Metamorphism (geology) ; Mica ; Micas ; Microscopy ; Mineralogy ; Minerals ; Muscovite ; Paleozoic ; Rock ; Rocks ; Software ; Stone ; Stratigraphy</subject><ispartof>Minerals (Basel), 2022-09, Vol.12 (9), p.1088</ispartof><rights>2022 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-c256t-b187c2c8f74db9dd38cd47d231579707f43acc7a653901deb9a219d58611f8bc3</cites><orcidid>0000-0002-8474-8600</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,776,780,27901,27902</link.rule.ids></links><search><creatorcontrib>Bozkaya, Ömer</creatorcontrib><creatorcontrib>Yalçın, Hüseyin</creatorcontrib><title>Mineral Chemistry of Low-Temperature Phyllosilicates in Early Paleozoic Metaclastic Rocks, Eastern Tauride Belt, Türkiye</title><title>Minerals (Basel)</title><description>The mineral chemistry of illite/mica and chlorites, together with the evaluation of textural data of low-temperature metaclastic rocks, plays an important role in determining their origin and metamorphic grade. This study aimed to investigate the chemical properties of phyllosilicates in early Paleozoic metaclastic rocks in the Eastern Tauride Belt, Türkiye. The textural (electron microscopy) and chemical (mineral chemistry analysis) analyses were performed on the samples representing different grades of metamorphism. The illites/micas and chlorites are observed as detrital (chlorite–mica stacks) and neoformation origin. Trioctahedral chlorites (chamosite) exhibit different chemistry for detrital and neoformed origin as well as the metamorphic grade. Tetrahedral Al and octahedral Fe + Mg increase, whereas octahedral Al decreases together with the increasing grade of metamorphism. The detrital chlorites have higher tetrahedral Al and Fe contents than their neoformed counterparts. Chlorite geothermometry data (detrital: 241–≥350 °C; neoformed: 201–268 °C) are compatible with the texture and illite Kübler index data. Illite/white-mica compositions display muscovite and Na-K mica. Tetrahedral Al and interlayer K + Na contents of illites/micas increase with metamorphic grade. Na-K mica and paragonite are observed as replacement-type developments within the detrital CMS. The obtained data indicate that phyllosilicate chemistry can be used effectively for determining the geological evolution of low-grade metamorphic sequences.</description><subject>Aluminum</subject><subject>Belts</subject><subject>Carbon</subject><subject>Chemical properties</subject><subject>Chemicophysical properties</subject><subject>Chemistry</subject><subject>Chlorite</subject><subject>Chlorites</subject><subject>Electron microscopy</subject><subject>Illite</subject><subject>Illites</subject><subject>Interlayers</subject><subject>Investigations</subject><subject>Iron</subject><subject>Laboratories</subject><subject>Low temperature</subject><subject>Magnesium</subject><subject>Metamorphism</subject><subject>Metamorphism (geology)</subject><subject>Mica</subject><subject>Micas</subject><subject>Microscopy</subject><subject>Mineralogy</subject><subject>Minerals</subject><subject>Muscovite</subject><subject>Paleozoic</subject><subject>Rock</subject><subject>Rocks</subject><subject>Software</subject><subject>Stone</subject><subject>Stratigraphy</subject><issn>2075-163X</issn><issn>2075-163X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2022</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNpNkF1LwzAUhoMoOOau_AMBL101H22TXuqYH7DhkArelTRJWbasmUmK1N_mnX_MyrzYuTkvvA_nwAPAJUY3lBbodmdaTFCBEecnYEQQyxKc0_fTo3wOJiFs0DAFpjwjI9AvTau9sHC21jsTou-ha-DCfSal3u2HJnZew9W6t9YFY40UUQdoWjgX3vZwJax2X85IuNRRSCtCHPKrk9swHZAQtW9hKTpvlIb32sYpLH--_db0-gKcNcIGPfnfY_D2MC9nT8ni5fF5drdIJMnymNSYM0kkb1iq6kIpyqVKmSIUZ6xgiDUpFVIykWeDA6x0XQiCC5XxHOOG15KOwdXh7t67j06HWG1c59vhZUUYzjOeEpIO1PWBkt6F4HVT7b3ZCd9XGFV_eqsjvfQXpR9vNw</recordid><startdate>20220901</startdate><enddate>20220901</enddate><creator>Bozkaya, Ömer</creator><creator>Yalçın, Hüseyin</creator><general>MDPI AG</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7TN</scope><scope>7UA</scope><scope>7WY</scope><scope>7WZ</scope><scope>7XB</scope><scope>87Z</scope><scope>8BQ</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>8FL</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BEZIV</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>D1I</scope><scope>DWQXO</scope><scope>F1W</scope><scope>FR3</scope><scope>FRNLG</scope><scope>F~G</scope><scope>H96</scope><scope>HCIFZ</scope><scope>JG9</scope><scope>K60</scope><scope>K6~</scope><scope>KB.</scope><scope>KR7</scope><scope>L.-</scope><scope>L.G</scope><scope>M0C</scope><scope>PCBAR</scope><scope>PDBOC</scope><scope>PIMPY</scope><scope>PQBIZ</scope><scope>PQBZA</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>Q9U</scope><orcidid>https://orcid.org/0000-0002-8474-8600</orcidid></search><sort><creationdate>20220901</creationdate><title>Mineral Chemistry of Low-Temperature Phyllosilicates in Early Paleozoic Metaclastic Rocks, Eastern Tauride Belt, Türkiye</title><author>Bozkaya, Ömer ; 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This study aimed to investigate the chemical properties of phyllosilicates in early Paleozoic metaclastic rocks in the Eastern Tauride Belt, Türkiye. The textural (electron microscopy) and chemical (mineral chemistry analysis) analyses were performed on the samples representing different grades of metamorphism. The illites/micas and chlorites are observed as detrital (chlorite–mica stacks) and neoformation origin. Trioctahedral chlorites (chamosite) exhibit different chemistry for detrital and neoformed origin as well as the metamorphic grade. Tetrahedral Al and octahedral Fe + Mg increase, whereas octahedral Al decreases together with the increasing grade of metamorphism. The detrital chlorites have higher tetrahedral Al and Fe contents than their neoformed counterparts. Chlorite geothermometry data (detrital: 241–≥350 °C; neoformed: 201–268 °C) are compatible with the texture and illite Kübler index data. Illite/white-mica compositions display muscovite and Na-K mica. Tetrahedral Al and interlayer K + Na contents of illites/micas increase with metamorphic grade. Na-K mica and paragonite are observed as replacement-type developments within the detrital CMS. The obtained data indicate that phyllosilicate chemistry can be used effectively for determining the geological evolution of low-grade metamorphic sequences.</abstract><cop>Basel</cop><pub>MDPI AG</pub><doi>10.3390/min12091088</doi><orcidid>https://orcid.org/0000-0002-8474-8600</orcidid><oa>free_for_read</oa></addata></record> |
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| subjects | Aluminum Belts Carbon Chemical properties Chemicophysical properties Chemistry Chlorite Chlorites Electron microscopy Illite Illites Interlayers Investigations Iron Laboratories Low temperature Magnesium Metamorphism Metamorphism (geology) Mica Micas Microscopy Mineralogy Minerals Muscovite Paleozoic Rock Rocks Software Stone Stratigraphy |
| title | Mineral Chemistry of Low-Temperature Phyllosilicates in Early Paleozoic Metaclastic Rocks, Eastern Tauride Belt, Türkiye |
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