Origin of dolomites in Lower-Middle Ordovician carbonate rocks in the Yingshan Formation, Gucheng Area, Tarim Basin: Evidence from petrography and geochemical data

Various degrees of dolomitization are widely present in the Yingshan Formation in the Gucheng area of the Tarim Basin. To determine the petrological characteristics and origin of the massive dolomites present, a rich combination of tools was well used, including previous research results, core and t...
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Autor*in:	Huang, Baiwen [verfasserIn] Zhang, Shaonan [verfasserIn] Lu, Ziye [verfasserIn] Ye, Ning [verfasserIn] Zhu, Bei [verfasserIn] Ding, Xiaoqi [verfasserIn] Li, Yingtao [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2021

Schlagwörter:	Dolomitization Recrystallization Carbon and oxygen isotopes Strontium isotopes Strontium content Yingshan formation

Übergeordnetes Werk:	Enthalten in: Marine and petroleum geology - Amsterdam [u.a.] : Elsevier Science, 1984, 134
Übergeordnetes Werk:	volume:134

DOI / URN:	10.1016/j.marpetgeo.2021.105322

Katalog-ID:	ELV006869971

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245	1	0	\|a Origin of dolomites in Lower-Middle Ordovician carbonate rocks in the Yingshan Formation, Gucheng Area, Tarim Basin: Evidence from petrography and geochemical data
264		1	\|c 2021
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520			\|a Various degrees of dolomitization are widely present in the Yingshan Formation in the Gucheng area of the Tarim Basin. To determine the petrological characteristics and origin of the massive dolomites present, a rich combination of tools was well used, including previous research results, core and thin-section samples, cathodoluminescence, carbon (C-) and oxygen (O-) isotopes, strontium (Sr-) isotopes and content, and burial-thermal history data. The results of this analysis successfully reveal three primary matrix dolomites and three special cements, as follows: (1) microcrystalline to very fine crystalline nonplanar-a dolomite (MD1); (2) very fine to fine crystalline planar-s to planar-e dolomite (MD2); (3) medium to coarse crystalline nonplanar-a to planar-s dolomite (MD3); (4) coarse crystalline nonplanar-a saddle dolomite cement (SD) and (5) medium to coarse crystalline calcite cements (C1 and C2). Among them, MD1 precipitated from the reflux of mildly evaporated seawater, and MD2 was formed by the first significant recrystallization of MD1 in shallow burial environments. In particular, some MD3 was formed by the second significant recrystallization of MD1 in medium-burial environments. The others, even SD, were likely the products of the third significant recrystallization and cementation in deep-burial environments that precipitate under the action of a hydrothermal fluid mixture composed of mantle-derived fluid and Cambrian thermal brine. In addition, C1 and C2 would form close to the times in which the Himalayan and Late Caledonian–Early Hercynian hydrocarbon charging events occurred, respectively.
650		4	\|a Dolomitization
650		4	\|a Recrystallization
650		4	\|a Carbon and oxygen isotopes
650		4	\|a Strontium isotopes
650		4	\|a Strontium content
650		4	\|a Yingshan formation
700	1		\|a Zhang, Shaonan \|e verfasserin \|4 aut
700	1		\|a Lu, Ziye \|e verfasserin \|4 aut
700	1		\|a Ye, Ning \|e verfasserin \|4 aut
700	1		\|a Zhu, Bei \|e verfasserin \|4 aut
700	1		\|a Ding, Xiaoqi \|e verfasserin \|4 aut
700	1		\|a Li, Yingtao \|e verfasserin \|4 aut
773	0	8	\|i Enthalten in \|t Marine and petroleum geology \|d Amsterdam [u.a.] : Elsevier Science, 1984 \|g 134 \|h Online-Ressource \|w (DE-627)303393416 \|w (DE-600)1494910-6 \|w (DE-576)259484032 \|x 0264-8172 \|7 nnns
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936	b	k	\|a 38.48 \|j Marine Geologie
936	b	k	\|a 38.51 \|j Geologie fossiler Brennstoffe
951			\|a AR
952			\|d 134

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author_variant	b h bh s z sz z l zl n y ny b z bz x d xd y l yl
matchkey_str	article:02648172:2021----::rgnfooieilwrideroiinabntrcsnhynsafrainuhnaetrmaieie
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publishDate	2021
allfields	10.1016/j.marpetgeo.2021.105322 doi (DE-627)ELV006869971 (ELSEVIER)S0264-8172(21)00425-6 DE-627 ger DE-627 rda eng 550 DE-600 38.48 bkl 38.51 bkl Huang, Baiwen verfasserin aut Origin of dolomites in Lower-Middle Ordovician carbonate rocks in the Yingshan Formation, Gucheng Area, Tarim Basin: Evidence from petrography and geochemical data 2021 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Various degrees of dolomitization are widely present in the Yingshan Formation in the Gucheng area of the Tarim Basin. To determine the petrological characteristics and origin of the massive dolomites present, a rich combination of tools was well used, including previous research results, core and thin-section samples, cathodoluminescence, carbon (C-) and oxygen (O-) isotopes, strontium (Sr-) isotopes and content, and burial-thermal history data. The results of this analysis successfully reveal three primary matrix dolomites and three special cements, as follows: (1) microcrystalline to very fine crystalline nonplanar-a dolomite (MD1); (2) very fine to fine crystalline planar-s to planar-e dolomite (MD2); (3) medium to coarse crystalline nonplanar-a to planar-s dolomite (MD3); (4) coarse crystalline nonplanar-a saddle dolomite cement (SD) and (5) medium to coarse crystalline calcite cements (C1 and C2). Among them, MD1 precipitated from the reflux of mildly evaporated seawater, and MD2 was formed by the first significant recrystallization of MD1 in shallow burial environments. In particular, some MD3 was formed by the second significant recrystallization of MD1 in medium-burial environments. The others, even SD, were likely the products of the third significant recrystallization and cementation in deep-burial environments that precipitate under the action of a hydrothermal fluid mixture composed of mantle-derived fluid and Cambrian thermal brine. In addition, C1 and C2 would form close to the times in which the Himalayan and Late Caledonian–Early Hercynian hydrocarbon charging events occurred, respectively. Dolomitization Recrystallization Carbon and oxygen isotopes Strontium isotopes Strontium content Yingshan formation Zhang, Shaonan verfasserin aut Lu, Ziye verfasserin aut Ye, Ning verfasserin aut Zhu, Bei verfasserin aut Ding, Xiaoqi verfasserin aut Li, Yingtao verfasserin aut Enthalten in Marine and petroleum geology Amsterdam [u.a.] : Elsevier Science, 1984 134 Online-Ressource (DE-627)303393416 (DE-600)1494910-6 (DE-576)259484032 0264-8172 nnns volume:134 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.48 Marine Geologie 38.51 Geologie fossiler Brennstoffe AR 134
spelling	10.1016/j.marpetgeo.2021.105322 doi (DE-627)ELV006869971 (ELSEVIER)S0264-8172(21)00425-6 DE-627 ger DE-627 rda eng 550 DE-600 38.48 bkl 38.51 bkl Huang, Baiwen verfasserin aut Origin of dolomites in Lower-Middle Ordovician carbonate rocks in the Yingshan Formation, Gucheng Area, Tarim Basin: Evidence from petrography and geochemical data 2021 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Various degrees of dolomitization are widely present in the Yingshan Formation in the Gucheng area of the Tarim Basin. To determine the petrological characteristics and origin of the massive dolomites present, a rich combination of tools was well used, including previous research results, core and thin-section samples, cathodoluminescence, carbon (C-) and oxygen (O-) isotopes, strontium (Sr-) isotopes and content, and burial-thermal history data. The results of this analysis successfully reveal three primary matrix dolomites and three special cements, as follows: (1) microcrystalline to very fine crystalline nonplanar-a dolomite (MD1); (2) very fine to fine crystalline planar-s to planar-e dolomite (MD2); (3) medium to coarse crystalline nonplanar-a to planar-s dolomite (MD3); (4) coarse crystalline nonplanar-a saddle dolomite cement (SD) and (5) medium to coarse crystalline calcite cements (C1 and C2). Among them, MD1 precipitated from the reflux of mildly evaporated seawater, and MD2 was formed by the first significant recrystallization of MD1 in shallow burial environments. In particular, some MD3 was formed by the second significant recrystallization of MD1 in medium-burial environments. The others, even SD, were likely the products of the third significant recrystallization and cementation in deep-burial environments that precipitate under the action of a hydrothermal fluid mixture composed of mantle-derived fluid and Cambrian thermal brine. In addition, C1 and C2 would form close to the times in which the Himalayan and Late Caledonian–Early Hercynian hydrocarbon charging events occurred, respectively. Dolomitization Recrystallization Carbon and oxygen isotopes Strontium isotopes Strontium content Yingshan formation Zhang, Shaonan verfasserin aut Lu, Ziye verfasserin aut Ye, Ning verfasserin aut Zhu, Bei verfasserin aut Ding, Xiaoqi verfasserin aut Li, Yingtao verfasserin aut Enthalten in Marine and petroleum geology Amsterdam [u.a.] : Elsevier Science, 1984 134 Online-Ressource (DE-627)303393416 (DE-600)1494910-6 (DE-576)259484032 0264-8172 nnns volume:134 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.48 Marine Geologie 38.51 Geologie fossiler Brennstoffe AR 134
allfields_unstemmed	10.1016/j.marpetgeo.2021.105322 doi (DE-627)ELV006869971 (ELSEVIER)S0264-8172(21)00425-6 DE-627 ger DE-627 rda eng 550 DE-600 38.48 bkl 38.51 bkl Huang, Baiwen verfasserin aut Origin of dolomites in Lower-Middle Ordovician carbonate rocks in the Yingshan Formation, Gucheng Area, Tarim Basin: Evidence from petrography and geochemical data 2021 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Various degrees of dolomitization are widely present in the Yingshan Formation in the Gucheng area of the Tarim Basin. To determine the petrological characteristics and origin of the massive dolomites present, a rich combination of tools was well used, including previous research results, core and thin-section samples, cathodoluminescence, carbon (C-) and oxygen (O-) isotopes, strontium (Sr-) isotopes and content, and burial-thermal history data. The results of this analysis successfully reveal three primary matrix dolomites and three special cements, as follows: (1) microcrystalline to very fine crystalline nonplanar-a dolomite (MD1); (2) very fine to fine crystalline planar-s to planar-e dolomite (MD2); (3) medium to coarse crystalline nonplanar-a to planar-s dolomite (MD3); (4) coarse crystalline nonplanar-a saddle dolomite cement (SD) and (5) medium to coarse crystalline calcite cements (C1 and C2). Among them, MD1 precipitated from the reflux of mildly evaporated seawater, and MD2 was formed by the first significant recrystallization of MD1 in shallow burial environments. In particular, some MD3 was formed by the second significant recrystallization of MD1 in medium-burial environments. The others, even SD, were likely the products of the third significant recrystallization and cementation in deep-burial environments that precipitate under the action of a hydrothermal fluid mixture composed of mantle-derived fluid and Cambrian thermal brine. In addition, C1 and C2 would form close to the times in which the Himalayan and Late Caledonian–Early Hercynian hydrocarbon charging events occurred, respectively. Dolomitization Recrystallization Carbon and oxygen isotopes Strontium isotopes Strontium content Yingshan formation Zhang, Shaonan verfasserin aut Lu, Ziye verfasserin aut Ye, Ning verfasserin aut Zhu, Bei verfasserin aut Ding, Xiaoqi verfasserin aut Li, Yingtao verfasserin aut Enthalten in Marine and petroleum geology Amsterdam [u.a.] : Elsevier Science, 1984 134 Online-Ressource (DE-627)303393416 (DE-600)1494910-6 (DE-576)259484032 0264-8172 nnns volume:134 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.48 Marine Geologie 38.51 Geologie fossiler Brennstoffe AR 134
allfieldsGer	10.1016/j.marpetgeo.2021.105322 doi (DE-627)ELV006869971 (ELSEVIER)S0264-8172(21)00425-6 DE-627 ger DE-627 rda eng 550 DE-600 38.48 bkl 38.51 bkl Huang, Baiwen verfasserin aut Origin of dolomites in Lower-Middle Ordovician carbonate rocks in the Yingshan Formation, Gucheng Area, Tarim Basin: Evidence from petrography and geochemical data 2021 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Various degrees of dolomitization are widely present in the Yingshan Formation in the Gucheng area of the Tarim Basin. To determine the petrological characteristics and origin of the massive dolomites present, a rich combination of tools was well used, including previous research results, core and thin-section samples, cathodoluminescence, carbon (C-) and oxygen (O-) isotopes, strontium (Sr-) isotopes and content, and burial-thermal history data. The results of this analysis successfully reveal three primary matrix dolomites and three special cements, as follows: (1) microcrystalline to very fine crystalline nonplanar-a dolomite (MD1); (2) very fine to fine crystalline planar-s to planar-e dolomite (MD2); (3) medium to coarse crystalline nonplanar-a to planar-s dolomite (MD3); (4) coarse crystalline nonplanar-a saddle dolomite cement (SD) and (5) medium to coarse crystalline calcite cements (C1 and C2). Among them, MD1 precipitated from the reflux of mildly evaporated seawater, and MD2 was formed by the first significant recrystallization of MD1 in shallow burial environments. In particular, some MD3 was formed by the second significant recrystallization of MD1 in medium-burial environments. The others, even SD, were likely the products of the third significant recrystallization and cementation in deep-burial environments that precipitate under the action of a hydrothermal fluid mixture composed of mantle-derived fluid and Cambrian thermal brine. In addition, C1 and C2 would form close to the times in which the Himalayan and Late Caledonian–Early Hercynian hydrocarbon charging events occurred, respectively. Dolomitization Recrystallization Carbon and oxygen isotopes Strontium isotopes Strontium content Yingshan formation Zhang, Shaonan verfasserin aut Lu, Ziye verfasserin aut Ye, Ning verfasserin aut Zhu, Bei verfasserin aut Ding, Xiaoqi verfasserin aut Li, Yingtao verfasserin aut Enthalten in Marine and petroleum geology Amsterdam [u.a.] : Elsevier Science, 1984 134 Online-Ressource (DE-627)303393416 (DE-600)1494910-6 (DE-576)259484032 0264-8172 nnns volume:134 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.48 Marine Geologie 38.51 Geologie fossiler Brennstoffe AR 134
allfieldsSound	10.1016/j.marpetgeo.2021.105322 doi (DE-627)ELV006869971 (ELSEVIER)S0264-8172(21)00425-6 DE-627 ger DE-627 rda eng 550 DE-600 38.48 bkl 38.51 bkl Huang, Baiwen verfasserin aut Origin of dolomites in Lower-Middle Ordovician carbonate rocks in the Yingshan Formation, Gucheng Area, Tarim Basin: Evidence from petrography and geochemical data 2021 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Various degrees of dolomitization are widely present in the Yingshan Formation in the Gucheng area of the Tarim Basin. To determine the petrological characteristics and origin of the massive dolomites present, a rich combination of tools was well used, including previous research results, core and thin-section samples, cathodoluminescence, carbon (C-) and oxygen (O-) isotopes, strontium (Sr-) isotopes and content, and burial-thermal history data. The results of this analysis successfully reveal three primary matrix dolomites and three special cements, as follows: (1) microcrystalline to very fine crystalline nonplanar-a dolomite (MD1); (2) very fine to fine crystalline planar-s to planar-e dolomite (MD2); (3) medium to coarse crystalline nonplanar-a to planar-s dolomite (MD3); (4) coarse crystalline nonplanar-a saddle dolomite cement (SD) and (5) medium to coarse crystalline calcite cements (C1 and C2). Among them, MD1 precipitated from the reflux of mildly evaporated seawater, and MD2 was formed by the first significant recrystallization of MD1 in shallow burial environments. In particular, some MD3 was formed by the second significant recrystallization of MD1 in medium-burial environments. The others, even SD, were likely the products of the third significant recrystallization and cementation in deep-burial environments that precipitate under the action of a hydrothermal fluid mixture composed of mantle-derived fluid and Cambrian thermal brine. In addition, C1 and C2 would form close to the times in which the Himalayan and Late Caledonian–Early Hercynian hydrocarbon charging events occurred, respectively. Dolomitization Recrystallization Carbon and oxygen isotopes Strontium isotopes Strontium content Yingshan formation Zhang, Shaonan verfasserin aut Lu, Ziye verfasserin aut Ye, Ning verfasserin aut Zhu, Bei verfasserin aut Ding, Xiaoqi verfasserin aut Li, Yingtao verfasserin aut Enthalten in Marine and petroleum geology Amsterdam [u.a.] : Elsevier Science, 1984 134 Online-Ressource (DE-627)303393416 (DE-600)1494910-6 (DE-576)259484032 0264-8172 nnns volume:134 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.48 Marine Geologie 38.51 Geologie fossiler Brennstoffe AR 134
language	English
source	Enthalten in Marine and petroleum geology 134 volume:134
sourceStr	Enthalten in Marine and petroleum geology 134 volume:134
format_phy_str_mv	Article
bklname	Marine Geologie Geologie fossiler Brennstoffe
institution	findex.gbv.de
topic_facet	Dolomitization Recrystallization Carbon and oxygen isotopes Strontium isotopes Strontium content Yingshan formation
dewey-raw	550
isfreeaccess_bool	false
container_title	Marine and petroleum geology
authorswithroles_txt_mv	Huang, Baiwen @@aut@@ Zhang, Shaonan @@aut@@ Lu, Ziye @@aut@@ Ye, Ning @@aut@@ Zhu, Bei @@aut@@ Ding, Xiaoqi @@aut@@ Li, Yingtao @@aut@@
publishDateDaySort_date	2021-01-01T00:00:00Z
hierarchy_top_id	303393416
dewey-sort	3550
id	ELV006869971
language_de	englisch
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author	Huang, Baiwen
spellingShingle	Huang, Baiwen ddc 550 bkl 38.48 bkl 38.51 misc Dolomitization misc Recrystallization misc Carbon and oxygen isotopes misc Strontium isotopes misc Strontium content misc Yingshan formation Origin of dolomites in Lower-Middle Ordovician carbonate rocks in the Yingshan Formation, Gucheng Area, Tarim Basin: Evidence from petrography and geochemical data
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topic_title	550 DE-600 38.48 bkl 38.51 bkl Origin of dolomites in Lower-Middle Ordovician carbonate rocks in the Yingshan Formation, Gucheng Area, Tarim Basin: Evidence from petrography and geochemical data Dolomitization Recrystallization Carbon and oxygen isotopes Strontium isotopes Strontium content Yingshan formation
topic	ddc 550 bkl 38.48 bkl 38.51 misc Dolomitization misc Recrystallization misc Carbon and oxygen isotopes misc Strontium isotopes misc Strontium content misc Yingshan formation
topic_unstemmed	ddc 550 bkl 38.48 bkl 38.51 misc Dolomitization misc Recrystallization misc Carbon and oxygen isotopes misc Strontium isotopes misc Strontium content misc Yingshan formation
topic_browse	ddc 550 bkl 38.48 bkl 38.51 misc Dolomitization misc Recrystallization misc Carbon and oxygen isotopes misc Strontium isotopes misc Strontium content misc Yingshan formation
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title	Origin of dolomites in Lower-Middle Ordovician carbonate rocks in the Yingshan Formation, Gucheng Area, Tarim Basin: Evidence from petrography and geochemical data
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title_full	Origin of dolomites in Lower-Middle Ordovician carbonate rocks in the Yingshan Formation, Gucheng Area, Tarim Basin: Evidence from petrography and geochemical data
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author_browse	Huang, Baiwen Zhang, Shaonan Lu, Ziye Ye, Ning Zhu, Bei Ding, Xiaoqi Li, Yingtao
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title_sort	origin of dolomites in lower-middle ordovician carbonate rocks in the yingshan formation, gucheng area, tarim basin: evidence from petrography and geochemical data
title_auth	Origin of dolomites in Lower-Middle Ordovician carbonate rocks in the Yingshan Formation, Gucheng Area, Tarim Basin: Evidence from petrography and geochemical data
abstract	Various degrees of dolomitization are widely present in the Yingshan Formation in the Gucheng area of the Tarim Basin. To determine the petrological characteristics and origin of the massive dolomites present, a rich combination of tools was well used, including previous research results, core and thin-section samples, cathodoluminescence, carbon (C-) and oxygen (O-) isotopes, strontium (Sr-) isotopes and content, and burial-thermal history data. The results of this analysis successfully reveal three primary matrix dolomites and three special cements, as follows: (1) microcrystalline to very fine crystalline nonplanar-a dolomite (MD1); (2) very fine to fine crystalline planar-s to planar-e dolomite (MD2); (3) medium to coarse crystalline nonplanar-a to planar-s dolomite (MD3); (4) coarse crystalline nonplanar-a saddle dolomite cement (SD) and (5) medium to coarse crystalline calcite cements (C1 and C2). Among them, MD1 precipitated from the reflux of mildly evaporated seawater, and MD2 was formed by the first significant recrystallization of MD1 in shallow burial environments. In particular, some MD3 was formed by the second significant recrystallization of MD1 in medium-burial environments. The others, even SD, were likely the products of the third significant recrystallization and cementation in deep-burial environments that precipitate under the action of a hydrothermal fluid mixture composed of mantle-derived fluid and Cambrian thermal brine. In addition, C1 and C2 would form close to the times in which the Himalayan and Late Caledonian–Early Hercynian hydrocarbon charging events occurred, respectively.
abstractGer	Various degrees of dolomitization are widely present in the Yingshan Formation in the Gucheng area of the Tarim Basin. To determine the petrological characteristics and origin of the massive dolomites present, a rich combination of tools was well used, including previous research results, core and thin-section samples, cathodoluminescence, carbon (C-) and oxygen (O-) isotopes, strontium (Sr-) isotopes and content, and burial-thermal history data. The results of this analysis successfully reveal three primary matrix dolomites and three special cements, as follows: (1) microcrystalline to very fine crystalline nonplanar-a dolomite (MD1); (2) very fine to fine crystalline planar-s to planar-e dolomite (MD2); (3) medium to coarse crystalline nonplanar-a to planar-s dolomite (MD3); (4) coarse crystalline nonplanar-a saddle dolomite cement (SD) and (5) medium to coarse crystalline calcite cements (C1 and C2). Among them, MD1 precipitated from the reflux of mildly evaporated seawater, and MD2 was formed by the first significant recrystallization of MD1 in shallow burial environments. In particular, some MD3 was formed by the second significant recrystallization of MD1 in medium-burial environments. The others, even SD, were likely the products of the third significant recrystallization and cementation in deep-burial environments that precipitate under the action of a hydrothermal fluid mixture composed of mantle-derived fluid and Cambrian thermal brine. In addition, C1 and C2 would form close to the times in which the Himalayan and Late Caledonian–Early Hercynian hydrocarbon charging events occurred, respectively.
abstract_unstemmed	Various degrees of dolomitization are widely present in the Yingshan Formation in the Gucheng area of the Tarim Basin. To determine the petrological characteristics and origin of the massive dolomites present, a rich combination of tools was well used, including previous research results, core and thin-section samples, cathodoluminescence, carbon (C-) and oxygen (O-) isotopes, strontium (Sr-) isotopes and content, and burial-thermal history data. The results of this analysis successfully reveal three primary matrix dolomites and three special cements, as follows: (1) microcrystalline to very fine crystalline nonplanar-a dolomite (MD1); (2) very fine to fine crystalline planar-s to planar-e dolomite (MD2); (3) medium to coarse crystalline nonplanar-a to planar-s dolomite (MD3); (4) coarse crystalline nonplanar-a saddle dolomite cement (SD) and (5) medium to coarse crystalline calcite cements (C1 and C2). Among them, MD1 precipitated from the reflux of mildly evaporated seawater, and MD2 was formed by the first significant recrystallization of MD1 in shallow burial environments. In particular, some MD3 was formed by the second significant recrystallization of MD1 in medium-burial environments. The others, even SD, were likely the products of the third significant recrystallization and cementation in deep-burial environments that precipitate under the action of a hydrothermal fluid mixture composed of mantle-derived fluid and Cambrian thermal brine. In addition, C1 and C2 would form close to the times in which the Himalayan and Late Caledonian–Early Hercynian hydrocarbon charging events occurred, respectively.
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title_short	Origin of dolomites in Lower-Middle Ordovician carbonate rocks in the Yingshan Formation, Gucheng Area, Tarim Basin: Evidence from petrography and geochemical data
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up_date	2024-07-06T22:49:56.523Z
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To determine the petrological characteristics and origin of the massive dolomites present, a rich combination of tools was well used, including previous research results, core and thin-section samples, cathodoluminescence, carbon (C-) and oxygen (O-) isotopes, strontium (Sr-) isotopes and content, and burial-thermal history data. The results of this analysis successfully reveal three primary matrix dolomites and three special cements, as follows: (1) microcrystalline to very fine crystalline nonplanar-a dolomite (MD1); (2) very fine to fine crystalline planar-s to planar-e dolomite (MD2); (3) medium to coarse crystalline nonplanar-a to planar-s dolomite (MD3); (4) coarse crystalline nonplanar-a saddle dolomite cement (SD) and (5) medium to coarse crystalline calcite cements (C1 and C2). Among them, MD1 precipitated from the reflux of mildly evaporated seawater, and MD2 was formed by the first significant recrystallization of MD1 in shallow burial environments. In particular, some MD3 was formed by the second significant recrystallization of MD1 in medium-burial environments. The others, even SD, were likely the products of the third significant recrystallization and cementation in deep-burial environments that precipitate under the action of a hydrothermal fluid mixture composed of mantle-derived fluid and Cambrian thermal brine. In addition, C1 and C2 would form close to the times in which the Himalayan and Late Caledonian–Early Hercynian hydrocarbon charging events occurred, respectively.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Dolomitization</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Recrystallization</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Carbon and oxygen isotopes</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Strontium isotopes</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Strontium content</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Yingshan formation</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Zhang, Shaonan</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield 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Origin of dolomites in Lower-Middle Ordovician carbonate rocks in the Yingshan Formation, Gucheng Area, Tarim Basin: Evidence from petrography and geochemical data

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