Morphological characteristics and growth influencing factors of Paleocene glauberite minerals in Jiangling Depression, China
Abstract Glauberite is the most common mineral in the ancient sodium sulphate deposits in the Jianghan Basin, although its origin, primary or diagenetic, continues to be a matter of debate. A number of glauberite deposits of Paleocene age in the Jiangling Depression display facies characteristics of...
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| Autor*in: |
Wang, Chunlian [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2022 |
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| Anmerkung: |
© The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2022 |
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| Übergeordnetes Werk: |
Enthalten in: Carbonates and evaporites - Springer Berlin Heidelberg, 1986, 37(2022), 2 vom: 16. Apr. |
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| Übergeordnetes Werk: |
volume:37 ; year:2022 ; number:2 ; day:16 ; month:04 |
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| DOI / URN: |
10.1007/s13146-022-00767-4 |
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OLC2078484814 |
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| 520 | |a Abstract Glauberite is the most common mineral in the ancient sodium sulphate deposits in the Jianghan Basin, although its origin, primary or diagenetic, continues to be a matter of debate. A number of glauberite deposits of Paleocene age in the Jiangling Depression display facies characteristics of sedimentologic significance. Based on field investigation and laboratory analysis, we determined three characteristics forms, rhombus I, rhombus II and long tabular shape. The glauberite crystal shapes in the south of Jiangling Depression mainly are macrocrystalline rhombus I and II, with the secondary amount of medium-grained crystal long tabular glauberite. This type of glauberite is interpreted as an unrest, shallow water and quickly crystallization, undergoing a strong evaporation along the lake basin boundary system. In the interior of the Jiangling Depression, glauberite assemblage is made up of fine-medium grained crystals of glauberite. The depositional environment is interpreted as a static and deeper water environment, which experienced a slow crystallization process. By studying morphology characteristics and depositional conditions of glauberite, we consider that different types of shapes and groups are the products of lake water evaporating under different climate conditions. Glauberite–halite lithofacies association is distinguished: association is composed of thin-bedded cloudy halite and thin-bedded glauberite. Transparent glauberite cemented by clear halite as well as normal-graded and reverse-graded glauberite textures are common. This type of transparent glauberite is interpreted as a primary, subaqueous precipitate. The glauberite in the Jiangling Depression are mainly stratified with typical rhythmic bedding, which is composed of the interaction between glauberite lamina and argillaceous dolomitic lamina or dolomitic argillaceous lamina. The tuberculous glauberite has remarkable top bending structure, which shows the penecontemporaneous in the process of its diagenesis. The evaporite cycle sequence of drillhole indicates that the brine of the salt lake in the south of Jiangling Depression is Na–K–Ca–Cl–$ SO_{4} $ type in the Paleocene. | ||
| 650 | 4 | |a Paleocene | |
| 650 | 4 | |a Jiangling Depression | |
| 650 | 4 | |a Glauberite | |
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| 700 | 1 | |a You, Chao |4 aut | |
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10.1007/s13146-022-00767-4 doi (DE-627)OLC2078484814 (DE-He213)s13146-022-00767-4-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Wang, Chunlian verfasserin aut Morphological characteristics and growth influencing factors of Paleocene glauberite minerals in Jiangling Depression, China 2022 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2022 Abstract Glauberite is the most common mineral in the ancient sodium sulphate deposits in the Jianghan Basin, although its origin, primary or diagenetic, continues to be a matter of debate. A number of glauberite deposits of Paleocene age in the Jiangling Depression display facies characteristics of sedimentologic significance. Based on field investigation and laboratory analysis, we determined three characteristics forms, rhombus I, rhombus II and long tabular shape. The glauberite crystal shapes in the south of Jiangling Depression mainly are macrocrystalline rhombus I and II, with the secondary amount of medium-grained crystal long tabular glauberite. This type of glauberite is interpreted as an unrest, shallow water and quickly crystallization, undergoing a strong evaporation along the lake basin boundary system. In the interior of the Jiangling Depression, glauberite assemblage is made up of fine-medium grained crystals of glauberite. The depositional environment is interpreted as a static and deeper water environment, which experienced a slow crystallization process. By studying morphology characteristics and depositional conditions of glauberite, we consider that different types of shapes and groups are the products of lake water evaporating under different climate conditions. Glauberite–halite lithofacies association is distinguished: association is composed of thin-bedded cloudy halite and thin-bedded glauberite. Transparent glauberite cemented by clear halite as well as normal-graded and reverse-graded glauberite textures are common. This type of transparent glauberite is interpreted as a primary, subaqueous precipitate. The glauberite in the Jiangling Depression are mainly stratified with typical rhythmic bedding, which is composed of the interaction between glauberite lamina and argillaceous dolomitic lamina or dolomitic argillaceous lamina. The tuberculous glauberite has remarkable top bending structure, which shows the penecontemporaneous in the process of its diagenesis. The evaporite cycle sequence of drillhole indicates that the brine of the salt lake in the south of Jiangling Depression is Na–K–Ca–Cl–$ SO_{4} $ type in the Paleocene. Paleocene Jiangling Depression Glauberite Evaporite Morphology characteristics Liu, Lihong (orcid)0000-0003-4332-4526 aut Yan, Kai aut Li, Ruiqin aut You, Chao aut Enthalten in Carbonates and evaporites Springer Berlin Heidelberg, 1986 37(2022), 2 vom: 16. Apr. (DE-627)165666978 (DE-600)1037732-3 (DE-576)09095369X 0891-2556 nnns volume:37 year:2022 number:2 day:16 month:04 https://doi.org/10.1007/s13146-022-00767-4 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_267 GBV_ILN_2018 GBV_ILN_4277 AR 37 2022 2 16 04 |
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10.1007/s13146-022-00767-4 doi (DE-627)OLC2078484814 (DE-He213)s13146-022-00767-4-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Wang, Chunlian verfasserin aut Morphological characteristics and growth influencing factors of Paleocene glauberite minerals in Jiangling Depression, China 2022 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2022 Abstract Glauberite is the most common mineral in the ancient sodium sulphate deposits in the Jianghan Basin, although its origin, primary or diagenetic, continues to be a matter of debate. A number of glauberite deposits of Paleocene age in the Jiangling Depression display facies characteristics of sedimentologic significance. Based on field investigation and laboratory analysis, we determined three characteristics forms, rhombus I, rhombus II and long tabular shape. The glauberite crystal shapes in the south of Jiangling Depression mainly are macrocrystalline rhombus I and II, with the secondary amount of medium-grained crystal long tabular glauberite. This type of glauberite is interpreted as an unrest, shallow water and quickly crystallization, undergoing a strong evaporation along the lake basin boundary system. In the interior of the Jiangling Depression, glauberite assemblage is made up of fine-medium grained crystals of glauberite. The depositional environment is interpreted as a static and deeper water environment, which experienced a slow crystallization process. By studying morphology characteristics and depositional conditions of glauberite, we consider that different types of shapes and groups are the products of lake water evaporating under different climate conditions. Glauberite–halite lithofacies association is distinguished: association is composed of thin-bedded cloudy halite and thin-bedded glauberite. Transparent glauberite cemented by clear halite as well as normal-graded and reverse-graded glauberite textures are common. This type of transparent glauberite is interpreted as a primary, subaqueous precipitate. The glauberite in the Jiangling Depression are mainly stratified with typical rhythmic bedding, which is composed of the interaction between glauberite lamina and argillaceous dolomitic lamina or dolomitic argillaceous lamina. The tuberculous glauberite has remarkable top bending structure, which shows the penecontemporaneous in the process of its diagenesis. The evaporite cycle sequence of drillhole indicates that the brine of the salt lake in the south of Jiangling Depression is Na–K–Ca–Cl–$ SO_{4} $ type in the Paleocene. Paleocene Jiangling Depression Glauberite Evaporite Morphology characteristics Liu, Lihong (orcid)0000-0003-4332-4526 aut Yan, Kai aut Li, Ruiqin aut You, Chao aut Enthalten in Carbonates and evaporites Springer Berlin Heidelberg, 1986 37(2022), 2 vom: 16. Apr. (DE-627)165666978 (DE-600)1037732-3 (DE-576)09095369X 0891-2556 nnns volume:37 year:2022 number:2 day:16 month:04 https://doi.org/10.1007/s13146-022-00767-4 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_267 GBV_ILN_2018 GBV_ILN_4277 AR 37 2022 2 16 04 |
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10.1007/s13146-022-00767-4 doi (DE-627)OLC2078484814 (DE-He213)s13146-022-00767-4-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Wang, Chunlian verfasserin aut Morphological characteristics and growth influencing factors of Paleocene glauberite minerals in Jiangling Depression, China 2022 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2022 Abstract Glauberite is the most common mineral in the ancient sodium sulphate deposits in the Jianghan Basin, although its origin, primary or diagenetic, continues to be a matter of debate. A number of glauberite deposits of Paleocene age in the Jiangling Depression display facies characteristics of sedimentologic significance. Based on field investigation and laboratory analysis, we determined three characteristics forms, rhombus I, rhombus II and long tabular shape. The glauberite crystal shapes in the south of Jiangling Depression mainly are macrocrystalline rhombus I and II, with the secondary amount of medium-grained crystal long tabular glauberite. This type of glauberite is interpreted as an unrest, shallow water and quickly crystallization, undergoing a strong evaporation along the lake basin boundary system. In the interior of the Jiangling Depression, glauberite assemblage is made up of fine-medium grained crystals of glauberite. The depositional environment is interpreted as a static and deeper water environment, which experienced a slow crystallization process. By studying morphology characteristics and depositional conditions of glauberite, we consider that different types of shapes and groups are the products of lake water evaporating under different climate conditions. Glauberite–halite lithofacies association is distinguished: association is composed of thin-bedded cloudy halite and thin-bedded glauberite. Transparent glauberite cemented by clear halite as well as normal-graded and reverse-graded glauberite textures are common. This type of transparent glauberite is interpreted as a primary, subaqueous precipitate. The glauberite in the Jiangling Depression are mainly stratified with typical rhythmic bedding, which is composed of the interaction between glauberite lamina and argillaceous dolomitic lamina or dolomitic argillaceous lamina. The tuberculous glauberite has remarkable top bending structure, which shows the penecontemporaneous in the process of its diagenesis. The evaporite cycle sequence of drillhole indicates that the brine of the salt lake in the south of Jiangling Depression is Na–K–Ca–Cl–$ SO_{4} $ type in the Paleocene. Paleocene Jiangling Depression Glauberite Evaporite Morphology characteristics Liu, Lihong (orcid)0000-0003-4332-4526 aut Yan, Kai aut Li, Ruiqin aut You, Chao aut Enthalten in Carbonates and evaporites Springer Berlin Heidelberg, 1986 37(2022), 2 vom: 16. Apr. (DE-627)165666978 (DE-600)1037732-3 (DE-576)09095369X 0891-2556 nnns volume:37 year:2022 number:2 day:16 month:04 https://doi.org/10.1007/s13146-022-00767-4 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_267 GBV_ILN_2018 GBV_ILN_4277 AR 37 2022 2 16 04 |
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10.1007/s13146-022-00767-4 doi (DE-627)OLC2078484814 (DE-He213)s13146-022-00767-4-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Wang, Chunlian verfasserin aut Morphological characteristics and growth influencing factors of Paleocene glauberite minerals in Jiangling Depression, China 2022 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2022 Abstract Glauberite is the most common mineral in the ancient sodium sulphate deposits in the Jianghan Basin, although its origin, primary or diagenetic, continues to be a matter of debate. A number of glauberite deposits of Paleocene age in the Jiangling Depression display facies characteristics of sedimentologic significance. Based on field investigation and laboratory analysis, we determined three characteristics forms, rhombus I, rhombus II and long tabular shape. The glauberite crystal shapes in the south of Jiangling Depression mainly are macrocrystalline rhombus I and II, with the secondary amount of medium-grained crystal long tabular glauberite. This type of glauberite is interpreted as an unrest, shallow water and quickly crystallization, undergoing a strong evaporation along the lake basin boundary system. In the interior of the Jiangling Depression, glauberite assemblage is made up of fine-medium grained crystals of glauberite. The depositional environment is interpreted as a static and deeper water environment, which experienced a slow crystallization process. By studying morphology characteristics and depositional conditions of glauberite, we consider that different types of shapes and groups are the products of lake water evaporating under different climate conditions. Glauberite–halite lithofacies association is distinguished: association is composed of thin-bedded cloudy halite and thin-bedded glauberite. Transparent glauberite cemented by clear halite as well as normal-graded and reverse-graded glauberite textures are common. This type of transparent glauberite is interpreted as a primary, subaqueous precipitate. The glauberite in the Jiangling Depression are mainly stratified with typical rhythmic bedding, which is composed of the interaction between glauberite lamina and argillaceous dolomitic lamina or dolomitic argillaceous lamina. The tuberculous glauberite has remarkable top bending structure, which shows the penecontemporaneous in the process of its diagenesis. The evaporite cycle sequence of drillhole indicates that the brine of the salt lake in the south of Jiangling Depression is Na–K–Ca–Cl–$ SO_{4} $ type in the Paleocene. Paleocene Jiangling Depression Glauberite Evaporite Morphology characteristics Liu, Lihong (orcid)0000-0003-4332-4526 aut Yan, Kai aut Li, Ruiqin aut You, Chao aut Enthalten in Carbonates and evaporites Springer Berlin Heidelberg, 1986 37(2022), 2 vom: 16. Apr. (DE-627)165666978 (DE-600)1037732-3 (DE-576)09095369X 0891-2556 nnns volume:37 year:2022 number:2 day:16 month:04 https://doi.org/10.1007/s13146-022-00767-4 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_267 GBV_ILN_2018 GBV_ILN_4277 AR 37 2022 2 16 04 |
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10.1007/s13146-022-00767-4 doi (DE-627)OLC2078484814 (DE-He213)s13146-022-00767-4-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Wang, Chunlian verfasserin aut Morphological characteristics and growth influencing factors of Paleocene glauberite minerals in Jiangling Depression, China 2022 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2022 Abstract Glauberite is the most common mineral in the ancient sodium sulphate deposits in the Jianghan Basin, although its origin, primary or diagenetic, continues to be a matter of debate. A number of glauberite deposits of Paleocene age in the Jiangling Depression display facies characteristics of sedimentologic significance. Based on field investigation and laboratory analysis, we determined three characteristics forms, rhombus I, rhombus II and long tabular shape. The glauberite crystal shapes in the south of Jiangling Depression mainly are macrocrystalline rhombus I and II, with the secondary amount of medium-grained crystal long tabular glauberite. This type of glauberite is interpreted as an unrest, shallow water and quickly crystallization, undergoing a strong evaporation along the lake basin boundary system. In the interior of the Jiangling Depression, glauberite assemblage is made up of fine-medium grained crystals of glauberite. The depositional environment is interpreted as a static and deeper water environment, which experienced a slow crystallization process. By studying morphology characteristics and depositional conditions of glauberite, we consider that different types of shapes and groups are the products of lake water evaporating under different climate conditions. Glauberite–halite lithofacies association is distinguished: association is composed of thin-bedded cloudy halite and thin-bedded glauberite. Transparent glauberite cemented by clear halite as well as normal-graded and reverse-graded glauberite textures are common. This type of transparent glauberite is interpreted as a primary, subaqueous precipitate. The glauberite in the Jiangling Depression are mainly stratified with typical rhythmic bedding, which is composed of the interaction between glauberite lamina and argillaceous dolomitic lamina or dolomitic argillaceous lamina. The tuberculous glauberite has remarkable top bending structure, which shows the penecontemporaneous in the process of its diagenesis. The evaporite cycle sequence of drillhole indicates that the brine of the salt lake in the south of Jiangling Depression is Na–K–Ca–Cl–$ SO_{4} $ type in the Paleocene. Paleocene Jiangling Depression Glauberite Evaporite Morphology characteristics Liu, Lihong (orcid)0000-0003-4332-4526 aut Yan, Kai aut Li, Ruiqin aut You, Chao aut Enthalten in Carbonates and evaporites Springer Berlin Heidelberg, 1986 37(2022), 2 vom: 16. Apr. (DE-627)165666978 (DE-600)1037732-3 (DE-576)09095369X 0891-2556 nnns volume:37 year:2022 number:2 day:16 month:04 https://doi.org/10.1007/s13146-022-00767-4 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_267 GBV_ILN_2018 GBV_ILN_4277 AR 37 2022 2 16 04 |
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morphological characteristics and growth influencing factors of paleocene glauberite minerals in jiangling depression, china |
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Morphological characteristics and growth influencing factors of Paleocene glauberite minerals in Jiangling Depression, China |
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Abstract Glauberite is the most common mineral in the ancient sodium sulphate deposits in the Jianghan Basin, although its origin, primary or diagenetic, continues to be a matter of debate. A number of glauberite deposits of Paleocene age in the Jiangling Depression display facies characteristics of sedimentologic significance. Based on field investigation and laboratory analysis, we determined three characteristics forms, rhombus I, rhombus II and long tabular shape. The glauberite crystal shapes in the south of Jiangling Depression mainly are macrocrystalline rhombus I and II, with the secondary amount of medium-grained crystal long tabular glauberite. This type of glauberite is interpreted as an unrest, shallow water and quickly crystallization, undergoing a strong evaporation along the lake basin boundary system. In the interior of the Jiangling Depression, glauberite assemblage is made up of fine-medium grained crystals of glauberite. The depositional environment is interpreted as a static and deeper water environment, which experienced a slow crystallization process. By studying morphology characteristics and depositional conditions of glauberite, we consider that different types of shapes and groups are the products of lake water evaporating under different climate conditions. Glauberite–halite lithofacies association is distinguished: association is composed of thin-bedded cloudy halite and thin-bedded glauberite. Transparent glauberite cemented by clear halite as well as normal-graded and reverse-graded glauberite textures are common. This type of transparent glauberite is interpreted as a primary, subaqueous precipitate. The glauberite in the Jiangling Depression are mainly stratified with typical rhythmic bedding, which is composed of the interaction between glauberite lamina and argillaceous dolomitic lamina or dolomitic argillaceous lamina. The tuberculous glauberite has remarkable top bending structure, which shows the penecontemporaneous in the process of its diagenesis. The evaporite cycle sequence of drillhole indicates that the brine of the salt lake in the south of Jiangling Depression is Na–K–Ca–Cl–$ SO_{4} $ type in the Paleocene. © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2022 |
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Abstract Glauberite is the most common mineral in the ancient sodium sulphate deposits in the Jianghan Basin, although its origin, primary or diagenetic, continues to be a matter of debate. A number of glauberite deposits of Paleocene age in the Jiangling Depression display facies characteristics of sedimentologic significance. Based on field investigation and laboratory analysis, we determined three characteristics forms, rhombus I, rhombus II and long tabular shape. The glauberite crystal shapes in the south of Jiangling Depression mainly are macrocrystalline rhombus I and II, with the secondary amount of medium-grained crystal long tabular glauberite. This type of glauberite is interpreted as an unrest, shallow water and quickly crystallization, undergoing a strong evaporation along the lake basin boundary system. In the interior of the Jiangling Depression, glauberite assemblage is made up of fine-medium grained crystals of glauberite. The depositional environment is interpreted as a static and deeper water environment, which experienced a slow crystallization process. By studying morphology characteristics and depositional conditions of glauberite, we consider that different types of shapes and groups are the products of lake water evaporating under different climate conditions. Glauberite–halite lithofacies association is distinguished: association is composed of thin-bedded cloudy halite and thin-bedded glauberite. Transparent glauberite cemented by clear halite as well as normal-graded and reverse-graded glauberite textures are common. This type of transparent glauberite is interpreted as a primary, subaqueous precipitate. The glauberite in the Jiangling Depression are mainly stratified with typical rhythmic bedding, which is composed of the interaction between glauberite lamina and argillaceous dolomitic lamina or dolomitic argillaceous lamina. The tuberculous glauberite has remarkable top bending structure, which shows the penecontemporaneous in the process of its diagenesis. The evaporite cycle sequence of drillhole indicates that the brine of the salt lake in the south of Jiangling Depression is Na–K–Ca–Cl–$ SO_{4} $ type in the Paleocene. © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2022 |
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Abstract Glauberite is the most common mineral in the ancient sodium sulphate deposits in the Jianghan Basin, although its origin, primary or diagenetic, continues to be a matter of debate. A number of glauberite deposits of Paleocene age in the Jiangling Depression display facies characteristics of sedimentologic significance. Based on field investigation and laboratory analysis, we determined three characteristics forms, rhombus I, rhombus II and long tabular shape. The glauberite crystal shapes in the south of Jiangling Depression mainly are macrocrystalline rhombus I and II, with the secondary amount of medium-grained crystal long tabular glauberite. This type of glauberite is interpreted as an unrest, shallow water and quickly crystallization, undergoing a strong evaporation along the lake basin boundary system. In the interior of the Jiangling Depression, glauberite assemblage is made up of fine-medium grained crystals of glauberite. The depositional environment is interpreted as a static and deeper water environment, which experienced a slow crystallization process. By studying morphology characteristics and depositional conditions of glauberite, we consider that different types of shapes and groups are the products of lake water evaporating under different climate conditions. Glauberite–halite lithofacies association is distinguished: association is composed of thin-bedded cloudy halite and thin-bedded glauberite. Transparent glauberite cemented by clear halite as well as normal-graded and reverse-graded glauberite textures are common. This type of transparent glauberite is interpreted as a primary, subaqueous precipitate. The glauberite in the Jiangling Depression are mainly stratified with typical rhythmic bedding, which is composed of the interaction between glauberite lamina and argillaceous dolomitic lamina or dolomitic argillaceous lamina. The tuberculous glauberite has remarkable top bending structure, which shows the penecontemporaneous in the process of its diagenesis. The evaporite cycle sequence of drillhole indicates that the brine of the salt lake in the south of Jiangling Depression is Na–K–Ca–Cl–$ SO_{4} $ type in the Paleocene. © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2022 |
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