Paleo-environmental constraints on uranium mineralization in the Ordos Basin: Evidence from the color zoning of U-bearing rock series
Color zoning of strata of Mesozoic continental basins in North China is closely correlated with the sedimentary environments of sandstone-type uranium deposits. Systematic research has been conducted on the colors of U-bearing rock series within the Ordos Basin by using data of several ten thousands...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Jin, Ruoshi [verfasserIn] Yu, Reng-An [verfasserIn] Yang, Jun [verfasserIn] Zhou, Xiaoxi [verfasserIn] Teng, Xueming [verfasserIn] Wang, Shanbo [verfasserIn] Si, Qinghong [verfasserIn] Zhu, Qiang [verfasserIn] Zhang, Tianfu [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2018 |
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| Schlagwörter: |
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| Übergeordnetes Werk: |
Enthalten in: Ore geology reviews - Amsterdam [u.a.] : Elsevier, 1986, 104, Seite 175-189 |
|---|---|
| Übergeordnetes Werk: |
volume:104 ; pages:175-189 |
| DOI / URN: |
10.1016/j.oregeorev.2018.10.016 |
|---|
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ELV009813039 |
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| 520 | |a Color zoning of strata of Mesozoic continental basins in North China is closely correlated with the sedimentary environments of sandstone-type uranium deposits. Systematic research has been conducted on the colors of U-bearing rock series within the Ordos Basin by using data of several ten thousands of drill holes from coal and oil fields. Taking an ore cluster as the unit, well-tie sections of deposit areas were compiled to analyze the vertical and lateral spatial variations in different color zones of rocks. Taking the basin as the unit, two typical well-tie sections in the central-northern basin were compiled in order to summarize the rock color zoning laws of U-bearing rock series within ore clusters and the entire basin. Lithogeochemical characteristics of different color zones in deposit areas and ore barren areas were studied. Especially, variations in trace elements in different color zones and the paleo-sedimentary environments they reflect were discussed. Within the Ordos Basin, from the basin margin to the center and from the U ore clusters to the ore barren areas, colors of the Zhiluo Formation U-bearing rock series generally display vertical zoning (i.e., from up downwards, red–green–gray [grayish black]) and show no lateral zoning characteristics. U ore beds mostly occur in the lower part of the green zone and the upper part of the gray zone. This conclusion differs greatly from the understanding on rock color zoning related to classic interlayer-oxidation-zone metallogenic theory. Hence, a correct understanding on color zoning of U-bearing rock series within the Ordos Basin is of great significance not only to U mineralization exploration but also to research on sandstone-type U mineralization theory. | ||
| 650 | 4 | |a Sandstone-type U mineralization | |
| 650 | 4 | |a U-bearing rock series | |
| 650 | 4 | |a Vertical zoning | |
| 650 | 4 | |a Paleo-sedimentary environment | |
| 650 | 4 | |a Ordos Basin | |
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10.1016/j.oregeorev.2018.10.016 doi (DE-627)ELV009813039 (ELSEVIER)S0169-1368(18)30299-3 DE-627 ger DE-627 rda eng 550 VZ 38.52 bkl 57.20 bkl Jin, Ruoshi verfasserin aut Paleo-environmental constraints on uranium mineralization in the Ordos Basin: Evidence from the color zoning of U-bearing rock series 2018 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Color zoning of strata of Mesozoic continental basins in North China is closely correlated with the sedimentary environments of sandstone-type uranium deposits. Systematic research has been conducted on the colors of U-bearing rock series within the Ordos Basin by using data of several ten thousands of drill holes from coal and oil fields. Taking an ore cluster as the unit, well-tie sections of deposit areas were compiled to analyze the vertical and lateral spatial variations in different color zones of rocks. Taking the basin as the unit, two typical well-tie sections in the central-northern basin were compiled in order to summarize the rock color zoning laws of U-bearing rock series within ore clusters and the entire basin. Lithogeochemical characteristics of different color zones in deposit areas and ore barren areas were studied. Especially, variations in trace elements in different color zones and the paleo-sedimentary environments they reflect were discussed. Within the Ordos Basin, from the basin margin to the center and from the U ore clusters to the ore barren areas, colors of the Zhiluo Formation U-bearing rock series generally display vertical zoning (i.e., from up downwards, red–green–gray [grayish black]) and show no lateral zoning characteristics. U ore beds mostly occur in the lower part of the green zone and the upper part of the gray zone. This conclusion differs greatly from the understanding on rock color zoning related to classic interlayer-oxidation-zone metallogenic theory. Hence, a correct understanding on color zoning of U-bearing rock series within the Ordos Basin is of great significance not only to U mineralization exploration but also to research on sandstone-type U mineralization theory. Sandstone-type U mineralization U-bearing rock series Vertical zoning Paleo-sedimentary environment Ordos Basin Yu, Reng-An verfasserin aut Yang, Jun verfasserin aut Zhou, Xiaoxi verfasserin aut Teng, Xueming verfasserin (orcid)0000-0003-3631-9892 aut Wang, Shanbo verfasserin aut Si, Qinghong verfasserin aut Zhu, Qiang verfasserin (orcid)0000-0002-2164-2753 aut Zhang, Tianfu verfasserin aut Enthalten in Ore geology reviews Amsterdam [u.a.] : Elsevier, 1986 104, Seite 175-189 Online-Ressource (DE-627)32461635X (DE-600)2029106-1 (DE-576)259485551 1872-7360 nnns volume:104 pages:175-189 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO SSG-OPC-GEO 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_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 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_2106 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_2232 GBV_ILN_2336 GBV_ILN_2470 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_4322 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 GBV_ILN_4700 38.52 Geologie der Erze VZ 57.20 Exploration und Prospektion von Bodenschätzen VZ AR 104 175-189 |
| spelling |
10.1016/j.oregeorev.2018.10.016 doi (DE-627)ELV009813039 (ELSEVIER)S0169-1368(18)30299-3 DE-627 ger DE-627 rda eng 550 VZ 38.52 bkl 57.20 bkl Jin, Ruoshi verfasserin aut Paleo-environmental constraints on uranium mineralization in the Ordos Basin: Evidence from the color zoning of U-bearing rock series 2018 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Color zoning of strata of Mesozoic continental basins in North China is closely correlated with the sedimentary environments of sandstone-type uranium deposits. Systematic research has been conducted on the colors of U-bearing rock series within the Ordos Basin by using data of several ten thousands of drill holes from coal and oil fields. Taking an ore cluster as the unit, well-tie sections of deposit areas were compiled to analyze the vertical and lateral spatial variations in different color zones of rocks. Taking the basin as the unit, two typical well-tie sections in the central-northern basin were compiled in order to summarize the rock color zoning laws of U-bearing rock series within ore clusters and the entire basin. Lithogeochemical characteristics of different color zones in deposit areas and ore barren areas were studied. Especially, variations in trace elements in different color zones and the paleo-sedimentary environments they reflect were discussed. Within the Ordos Basin, from the basin margin to the center and from the U ore clusters to the ore barren areas, colors of the Zhiluo Formation U-bearing rock series generally display vertical zoning (i.e., from up downwards, red–green–gray [grayish black]) and show no lateral zoning characteristics. U ore beds mostly occur in the lower part of the green zone and the upper part of the gray zone. This conclusion differs greatly from the understanding on rock color zoning related to classic interlayer-oxidation-zone metallogenic theory. Hence, a correct understanding on color zoning of U-bearing rock series within the Ordos Basin is of great significance not only to U mineralization exploration but also to research on sandstone-type U mineralization theory. Sandstone-type U mineralization U-bearing rock series Vertical zoning Paleo-sedimentary environment Ordos Basin Yu, Reng-An verfasserin aut Yang, Jun verfasserin aut Zhou, Xiaoxi verfasserin aut Teng, Xueming verfasserin (orcid)0000-0003-3631-9892 aut Wang, Shanbo verfasserin aut Si, Qinghong verfasserin aut Zhu, Qiang verfasserin (orcid)0000-0002-2164-2753 aut Zhang, Tianfu verfasserin aut Enthalten in Ore geology reviews Amsterdam [u.a.] : Elsevier, 1986 104, Seite 175-189 Online-Ressource (DE-627)32461635X (DE-600)2029106-1 (DE-576)259485551 1872-7360 nnns volume:104 pages:175-189 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO SSG-OPC-GEO 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_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 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_2106 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_2232 GBV_ILN_2336 GBV_ILN_2470 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_4322 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 GBV_ILN_4700 38.52 Geologie der Erze VZ 57.20 Exploration und Prospektion von Bodenschätzen VZ AR 104 175-189 |
| allfields_unstemmed |
10.1016/j.oregeorev.2018.10.016 doi (DE-627)ELV009813039 (ELSEVIER)S0169-1368(18)30299-3 DE-627 ger DE-627 rda eng 550 VZ 38.52 bkl 57.20 bkl Jin, Ruoshi verfasserin aut Paleo-environmental constraints on uranium mineralization in the Ordos Basin: Evidence from the color zoning of U-bearing rock series 2018 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Color zoning of strata of Mesozoic continental basins in North China is closely correlated with the sedimentary environments of sandstone-type uranium deposits. Systematic research has been conducted on the colors of U-bearing rock series within the Ordos Basin by using data of several ten thousands of drill holes from coal and oil fields. Taking an ore cluster as the unit, well-tie sections of deposit areas were compiled to analyze the vertical and lateral spatial variations in different color zones of rocks. Taking the basin as the unit, two typical well-tie sections in the central-northern basin were compiled in order to summarize the rock color zoning laws of U-bearing rock series within ore clusters and the entire basin. Lithogeochemical characteristics of different color zones in deposit areas and ore barren areas were studied. Especially, variations in trace elements in different color zones and the paleo-sedimentary environments they reflect were discussed. Within the Ordos Basin, from the basin margin to the center and from the U ore clusters to the ore barren areas, colors of the Zhiluo Formation U-bearing rock series generally display vertical zoning (i.e., from up downwards, red–green–gray [grayish black]) and show no lateral zoning characteristics. U ore beds mostly occur in the lower part of the green zone and the upper part of the gray zone. This conclusion differs greatly from the understanding on rock color zoning related to classic interlayer-oxidation-zone metallogenic theory. Hence, a correct understanding on color zoning of U-bearing rock series within the Ordos Basin is of great significance not only to U mineralization exploration but also to research on sandstone-type U mineralization theory. Sandstone-type U mineralization U-bearing rock series Vertical zoning Paleo-sedimentary environment Ordos Basin Yu, Reng-An verfasserin aut Yang, Jun verfasserin aut Zhou, Xiaoxi verfasserin aut Teng, Xueming verfasserin (orcid)0000-0003-3631-9892 aut Wang, Shanbo verfasserin aut Si, Qinghong verfasserin aut Zhu, Qiang verfasserin (orcid)0000-0002-2164-2753 aut Zhang, Tianfu verfasserin aut Enthalten in Ore geology reviews Amsterdam [u.a.] : Elsevier, 1986 104, Seite 175-189 Online-Ressource (DE-627)32461635X (DE-600)2029106-1 (DE-576)259485551 1872-7360 nnns volume:104 pages:175-189 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO SSG-OPC-GEO 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_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 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_2106 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_2232 GBV_ILN_2336 GBV_ILN_2470 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_4322 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 GBV_ILN_4700 38.52 Geologie der Erze VZ 57.20 Exploration und Prospektion von Bodenschätzen VZ AR 104 175-189 |
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10.1016/j.oregeorev.2018.10.016 doi (DE-627)ELV009813039 (ELSEVIER)S0169-1368(18)30299-3 DE-627 ger DE-627 rda eng 550 VZ 38.52 bkl 57.20 bkl Jin, Ruoshi verfasserin aut Paleo-environmental constraints on uranium mineralization in the Ordos Basin: Evidence from the color zoning of U-bearing rock series 2018 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Color zoning of strata of Mesozoic continental basins in North China is closely correlated with the sedimentary environments of sandstone-type uranium deposits. Systematic research has been conducted on the colors of U-bearing rock series within the Ordos Basin by using data of several ten thousands of drill holes from coal and oil fields. Taking an ore cluster as the unit, well-tie sections of deposit areas were compiled to analyze the vertical and lateral spatial variations in different color zones of rocks. Taking the basin as the unit, two typical well-tie sections in the central-northern basin were compiled in order to summarize the rock color zoning laws of U-bearing rock series within ore clusters and the entire basin. Lithogeochemical characteristics of different color zones in deposit areas and ore barren areas were studied. Especially, variations in trace elements in different color zones and the paleo-sedimentary environments they reflect were discussed. Within the Ordos Basin, from the basin margin to the center and from the U ore clusters to the ore barren areas, colors of the Zhiluo Formation U-bearing rock series generally display vertical zoning (i.e., from up downwards, red–green–gray [grayish black]) and show no lateral zoning characteristics. U ore beds mostly occur in the lower part of the green zone and the upper part of the gray zone. This conclusion differs greatly from the understanding on rock color zoning related to classic interlayer-oxidation-zone metallogenic theory. Hence, a correct understanding on color zoning of U-bearing rock series within the Ordos Basin is of great significance not only to U mineralization exploration but also to research on sandstone-type U mineralization theory. Sandstone-type U mineralization U-bearing rock series Vertical zoning Paleo-sedimentary environment Ordos Basin Yu, Reng-An verfasserin aut Yang, Jun verfasserin aut Zhou, Xiaoxi verfasserin aut Teng, Xueming verfasserin (orcid)0000-0003-3631-9892 aut Wang, Shanbo verfasserin aut Si, Qinghong verfasserin aut Zhu, Qiang verfasserin (orcid)0000-0002-2164-2753 aut Zhang, Tianfu verfasserin aut Enthalten in Ore geology reviews Amsterdam [u.a.] : Elsevier, 1986 104, Seite 175-189 Online-Ressource (DE-627)32461635X (DE-600)2029106-1 (DE-576)259485551 1872-7360 nnns volume:104 pages:175-189 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO SSG-OPC-GEO 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_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 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_2106 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_2232 GBV_ILN_2336 GBV_ILN_2470 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_4322 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 GBV_ILN_4700 38.52 Geologie der Erze VZ 57.20 Exploration und Prospektion von Bodenschätzen VZ AR 104 175-189 |
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10.1016/j.oregeorev.2018.10.016 doi (DE-627)ELV009813039 (ELSEVIER)S0169-1368(18)30299-3 DE-627 ger DE-627 rda eng 550 VZ 38.52 bkl 57.20 bkl Jin, Ruoshi verfasserin aut Paleo-environmental constraints on uranium mineralization in the Ordos Basin: Evidence from the color zoning of U-bearing rock series 2018 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Color zoning of strata of Mesozoic continental basins in North China is closely correlated with the sedimentary environments of sandstone-type uranium deposits. Systematic research has been conducted on the colors of U-bearing rock series within the Ordos Basin by using data of several ten thousands of drill holes from coal and oil fields. Taking an ore cluster as the unit, well-tie sections of deposit areas were compiled to analyze the vertical and lateral spatial variations in different color zones of rocks. Taking the basin as the unit, two typical well-tie sections in the central-northern basin were compiled in order to summarize the rock color zoning laws of U-bearing rock series within ore clusters and the entire basin. Lithogeochemical characteristics of different color zones in deposit areas and ore barren areas were studied. Especially, variations in trace elements in different color zones and the paleo-sedimentary environments they reflect were discussed. Within the Ordos Basin, from the basin margin to the center and from the U ore clusters to the ore barren areas, colors of the Zhiluo Formation U-bearing rock series generally display vertical zoning (i.e., from up downwards, red–green–gray [grayish black]) and show no lateral zoning characteristics. U ore beds mostly occur in the lower part of the green zone and the upper part of the gray zone. This conclusion differs greatly from the understanding on rock color zoning related to classic interlayer-oxidation-zone metallogenic theory. Hence, a correct understanding on color zoning of U-bearing rock series within the Ordos Basin is of great significance not only to U mineralization exploration but also to research on sandstone-type U mineralization theory. Sandstone-type U mineralization U-bearing rock series Vertical zoning Paleo-sedimentary environment Ordos Basin Yu, Reng-An verfasserin aut Yang, Jun verfasserin aut Zhou, Xiaoxi verfasserin aut Teng, Xueming verfasserin (orcid)0000-0003-3631-9892 aut Wang, Shanbo verfasserin aut Si, Qinghong verfasserin aut Zhu, Qiang verfasserin (orcid)0000-0002-2164-2753 aut Zhang, Tianfu verfasserin aut Enthalten in Ore geology reviews Amsterdam [u.a.] : Elsevier, 1986 104, Seite 175-189 Online-Ressource (DE-627)32461635X (DE-600)2029106-1 (DE-576)259485551 1872-7360 nnns volume:104 pages:175-189 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO SSG-OPC-GEO 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_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 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_2106 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_2232 GBV_ILN_2336 GBV_ILN_2470 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_4322 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 GBV_ILN_4700 38.52 Geologie der Erze VZ 57.20 Exploration und Prospektion von Bodenschätzen VZ AR 104 175-189 |
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Jin, Ruoshi |
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550 VZ 38.52 bkl 57.20 bkl Paleo-environmental constraints on uranium mineralization in the Ordos Basin: Evidence from the color zoning of U-bearing rock series Sandstone-type U mineralization U-bearing rock series Vertical zoning Paleo-sedimentary environment Ordos Basin |
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Paleo-environmental constraints on uranium mineralization in the Ordos Basin: Evidence from the color zoning of U-bearing rock series |
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paleo-environmental constraints on uranium mineralization in the ordos basin: evidence from the color zoning of u-bearing rock series |
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Paleo-environmental constraints on uranium mineralization in the Ordos Basin: Evidence from the color zoning of U-bearing rock series |
| abstract |
Color zoning of strata of Mesozoic continental basins in North China is closely correlated with the sedimentary environments of sandstone-type uranium deposits. Systematic research has been conducted on the colors of U-bearing rock series within the Ordos Basin by using data of several ten thousands of drill holes from coal and oil fields. Taking an ore cluster as the unit, well-tie sections of deposit areas were compiled to analyze the vertical and lateral spatial variations in different color zones of rocks. Taking the basin as the unit, two typical well-tie sections in the central-northern basin were compiled in order to summarize the rock color zoning laws of U-bearing rock series within ore clusters and the entire basin. Lithogeochemical characteristics of different color zones in deposit areas and ore barren areas were studied. Especially, variations in trace elements in different color zones and the paleo-sedimentary environments they reflect were discussed. Within the Ordos Basin, from the basin margin to the center and from the U ore clusters to the ore barren areas, colors of the Zhiluo Formation U-bearing rock series generally display vertical zoning (i.e., from up downwards, red–green–gray [grayish black]) and show no lateral zoning characteristics. U ore beds mostly occur in the lower part of the green zone and the upper part of the gray zone. This conclusion differs greatly from the understanding on rock color zoning related to classic interlayer-oxidation-zone metallogenic theory. Hence, a correct understanding on color zoning of U-bearing rock series within the Ordos Basin is of great significance not only to U mineralization exploration but also to research on sandstone-type U mineralization theory. |
| abstractGer |
Color zoning of strata of Mesozoic continental basins in North China is closely correlated with the sedimentary environments of sandstone-type uranium deposits. Systematic research has been conducted on the colors of U-bearing rock series within the Ordos Basin by using data of several ten thousands of drill holes from coal and oil fields. Taking an ore cluster as the unit, well-tie sections of deposit areas were compiled to analyze the vertical and lateral spatial variations in different color zones of rocks. Taking the basin as the unit, two typical well-tie sections in the central-northern basin were compiled in order to summarize the rock color zoning laws of U-bearing rock series within ore clusters and the entire basin. Lithogeochemical characteristics of different color zones in deposit areas and ore barren areas were studied. Especially, variations in trace elements in different color zones and the paleo-sedimentary environments they reflect were discussed. Within the Ordos Basin, from the basin margin to the center and from the U ore clusters to the ore barren areas, colors of the Zhiluo Formation U-bearing rock series generally display vertical zoning (i.e., from up downwards, red–green–gray [grayish black]) and show no lateral zoning characteristics. U ore beds mostly occur in the lower part of the green zone and the upper part of the gray zone. This conclusion differs greatly from the understanding on rock color zoning related to classic interlayer-oxidation-zone metallogenic theory. Hence, a correct understanding on color zoning of U-bearing rock series within the Ordos Basin is of great significance not only to U mineralization exploration but also to research on sandstone-type U mineralization theory. |
| abstract_unstemmed |
Color zoning of strata of Mesozoic continental basins in North China is closely correlated with the sedimentary environments of sandstone-type uranium deposits. Systematic research has been conducted on the colors of U-bearing rock series within the Ordos Basin by using data of several ten thousands of drill holes from coal and oil fields. Taking an ore cluster as the unit, well-tie sections of deposit areas were compiled to analyze the vertical and lateral spatial variations in different color zones of rocks. Taking the basin as the unit, two typical well-tie sections in the central-northern basin were compiled in order to summarize the rock color zoning laws of U-bearing rock series within ore clusters and the entire basin. Lithogeochemical characteristics of different color zones in deposit areas and ore barren areas were studied. Especially, variations in trace elements in different color zones and the paleo-sedimentary environments they reflect were discussed. Within the Ordos Basin, from the basin margin to the center and from the U ore clusters to the ore barren areas, colors of the Zhiluo Formation U-bearing rock series generally display vertical zoning (i.e., from up downwards, red–green–gray [grayish black]) and show no lateral zoning characteristics. U ore beds mostly occur in the lower part of the green zone and the upper part of the gray zone. This conclusion differs greatly from the understanding on rock color zoning related to classic interlayer-oxidation-zone metallogenic theory. Hence, a correct understanding on color zoning of U-bearing rock series within the Ordos Basin is of great significance not only to U mineralization exploration but also to research on sandstone-type U mineralization theory. |
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Within the Ordos Basin, from the basin margin to the center and from the U ore clusters to the ore barren areas, colors of the Zhiluo Formation U-bearing rock series generally display vertical zoning (i.e., from up downwards, red–green–gray [grayish black]) and show no lateral zoning characteristics. U ore beds mostly occur in the lower part of the green zone and the upper part of the gray zone. This conclusion differs greatly from the understanding on rock color zoning related to classic interlayer-oxidation-zone metallogenic theory. 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Jun</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Zhou, Xiaoxi</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Teng, Xueming</subfield><subfield code="e">verfasserin</subfield><subfield code="0">(orcid)0000-0003-3631-9892</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Wang, Shanbo</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Si, Qinghong</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Zhu, Qiang</subfield><subfield code="e">verfasserin</subfield><subfield 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