Textural characteristics of sediments and weathering in the Jhelum river basin located in Kashmir Valley, Western Himalaya
Abstract This study presents a detailed textural and geochemical study of sediments of river Jhelum and its tributaries of Kashmir valley. The textural studies clearly established that the sediments were dominantly of medium grain size, moderately sorted and very positively skewed. The kurtosis sugg...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Mir, Riyaz Ahmad [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2015 |
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| Schlagwörter: |
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| Anmerkung: |
© Geological Society of India 2015 |
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| Übergeordnetes Werk: |
Enthalten in: Journal of the Geological Society of India - New Delhi : Springer India, 1959, 86(2015), 4 vom: Okt., Seite 445-458 |
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| Übergeordnetes Werk: |
volume:86 ; year:2015 ; number:4 ; month:10 ; pages:445-458 |
| Links: |
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| DOI / URN: |
10.1007/s12594-015-0332-2 |
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SPR02621265X |
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| 520 | |a Abstract This study presents a detailed textural and geochemical study of sediments of river Jhelum and its tributaries of Kashmir valley. The textural studies clearly established that the sediments were dominantly of medium grain size, moderately sorted and very positively skewed. The kurtosis suggested dominantly leptokurtic nature of sediments. The sediments were deposited under moderate to low energy conditions with dominant rolling processes. The statistical parameters showed little spatial as well as temporal variations. The observations are supported by the frequency curves and bivariate plots between various textural parameters, confirming the polymodal nature of sediments with dominant to moderate sand fraction. The bimodal and unimodal nature of the sediments was also present at certain locations. The major oxide elemental chemistry of the sediments indicated that the dominant elemental oxide was $ SiO_{2} $ followed by $ Al_{2} %$ O_{3} $ in all the sediments. The Chemical Index Alteration (CIA) and Resistant Index of Maturity ($ R_{M} $) reflected moderate weathering and immaturity of the sediments in the basin. | ||
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10.1007/s12594-015-0332-2 doi (DE-627)SPR02621265X (SPR)s12594-015-0332-2-e DE-627 ger DE-627 rakwb eng Mir, Riyaz Ahmad verfasserin aut Textural characteristics of sediments and weathering in the Jhelum river basin located in Kashmir Valley, Western Himalaya 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Geological Society of India 2015 Abstract This study presents a detailed textural and geochemical study of sediments of river Jhelum and its tributaries of Kashmir valley. The textural studies clearly established that the sediments were dominantly of medium grain size, moderately sorted and very positively skewed. The kurtosis suggested dominantly leptokurtic nature of sediments. The sediments were deposited under moderate to low energy conditions with dominant rolling processes. The statistical parameters showed little spatial as well as temporal variations. The observations are supported by the frequency curves and bivariate plots between various textural parameters, confirming the polymodal nature of sediments with dominant to moderate sand fraction. The bimodal and unimodal nature of the sediments was also present at certain locations. The major oxide elemental chemistry of the sediments indicated that the dominant elemental oxide was $ SiO_{2} $ followed by $ Al_{2} %$ O_{3} $ in all the sediments. The Chemical Index Alteration (CIA) and Resistant Index of Maturity ($ R_{M} $) reflected moderate weathering and immaturity of the sediments in the basin. Grain size (dpeaa)DE-He213 Weathering (dpeaa)DE-He213 Jhelum (dpeaa)DE-He213 Kashmir valley (dpeaa)DE-He213 Himalaya (dpeaa)DE-He213 Jeelani, Gh aut Enthalten in Journal of the Geological Society of India New Delhi : Springer India, 1959 86(2015), 4 vom: Okt., Seite 445-458 (DE-627)60666078X (DE-600)2508930-4 0974-6889 nnns volume:86 year:2015 number:4 month:10 pages:445-458 https://dx.doi.org/10.1007/s12594-015-0332-2 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 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_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 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_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 86 2015 4 10 445-458 |
| spelling |
10.1007/s12594-015-0332-2 doi (DE-627)SPR02621265X (SPR)s12594-015-0332-2-e DE-627 ger DE-627 rakwb eng Mir, Riyaz Ahmad verfasserin aut Textural characteristics of sediments and weathering in the Jhelum river basin located in Kashmir Valley, Western Himalaya 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Geological Society of India 2015 Abstract This study presents a detailed textural and geochemical study of sediments of river Jhelum and its tributaries of Kashmir valley. The textural studies clearly established that the sediments were dominantly of medium grain size, moderately sorted and very positively skewed. The kurtosis suggested dominantly leptokurtic nature of sediments. The sediments were deposited under moderate to low energy conditions with dominant rolling processes. The statistical parameters showed little spatial as well as temporal variations. The observations are supported by the frequency curves and bivariate plots between various textural parameters, confirming the polymodal nature of sediments with dominant to moderate sand fraction. The bimodal and unimodal nature of the sediments was also present at certain locations. The major oxide elemental chemistry of the sediments indicated that the dominant elemental oxide was $ SiO_{2} $ followed by $ Al_{2} %$ O_{3} $ in all the sediments. The Chemical Index Alteration (CIA) and Resistant Index of Maturity ($ R_{M} $) reflected moderate weathering and immaturity of the sediments in the basin. Grain size (dpeaa)DE-He213 Weathering (dpeaa)DE-He213 Jhelum (dpeaa)DE-He213 Kashmir valley (dpeaa)DE-He213 Himalaya (dpeaa)DE-He213 Jeelani, Gh aut Enthalten in Journal of the Geological Society of India New Delhi : Springer India, 1959 86(2015), 4 vom: Okt., Seite 445-458 (DE-627)60666078X (DE-600)2508930-4 0974-6889 nnns volume:86 year:2015 number:4 month:10 pages:445-458 https://dx.doi.org/10.1007/s12594-015-0332-2 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 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_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 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_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 86 2015 4 10 445-458 |
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10.1007/s12594-015-0332-2 doi (DE-627)SPR02621265X (SPR)s12594-015-0332-2-e DE-627 ger DE-627 rakwb eng Mir, Riyaz Ahmad verfasserin aut Textural characteristics of sediments and weathering in the Jhelum river basin located in Kashmir Valley, Western Himalaya 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Geological Society of India 2015 Abstract This study presents a detailed textural and geochemical study of sediments of river Jhelum and its tributaries of Kashmir valley. The textural studies clearly established that the sediments were dominantly of medium grain size, moderately sorted and very positively skewed. The kurtosis suggested dominantly leptokurtic nature of sediments. The sediments were deposited under moderate to low energy conditions with dominant rolling processes. The statistical parameters showed little spatial as well as temporal variations. The observations are supported by the frequency curves and bivariate plots between various textural parameters, confirming the polymodal nature of sediments with dominant to moderate sand fraction. The bimodal and unimodal nature of the sediments was also present at certain locations. The major oxide elemental chemistry of the sediments indicated that the dominant elemental oxide was $ SiO_{2} $ followed by $ Al_{2} %$ O_{3} $ in all the sediments. The Chemical Index Alteration (CIA) and Resistant Index of Maturity ($ R_{M} $) reflected moderate weathering and immaturity of the sediments in the basin. Grain size (dpeaa)DE-He213 Weathering (dpeaa)DE-He213 Jhelum (dpeaa)DE-He213 Kashmir valley (dpeaa)DE-He213 Himalaya (dpeaa)DE-He213 Jeelani, Gh aut Enthalten in Journal of the Geological Society of India New Delhi : Springer India, 1959 86(2015), 4 vom: Okt., Seite 445-458 (DE-627)60666078X (DE-600)2508930-4 0974-6889 nnns volume:86 year:2015 number:4 month:10 pages:445-458 https://dx.doi.org/10.1007/s12594-015-0332-2 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 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_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 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_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 86 2015 4 10 445-458 |
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10.1007/s12594-015-0332-2 doi (DE-627)SPR02621265X (SPR)s12594-015-0332-2-e DE-627 ger DE-627 rakwb eng Mir, Riyaz Ahmad verfasserin aut Textural characteristics of sediments and weathering in the Jhelum river basin located in Kashmir Valley, Western Himalaya 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Geological Society of India 2015 Abstract This study presents a detailed textural and geochemical study of sediments of river Jhelum and its tributaries of Kashmir valley. The textural studies clearly established that the sediments were dominantly of medium grain size, moderately sorted and very positively skewed. The kurtosis suggested dominantly leptokurtic nature of sediments. The sediments were deposited under moderate to low energy conditions with dominant rolling processes. The statistical parameters showed little spatial as well as temporal variations. The observations are supported by the frequency curves and bivariate plots between various textural parameters, confirming the polymodal nature of sediments with dominant to moderate sand fraction. The bimodal and unimodal nature of the sediments was also present at certain locations. The major oxide elemental chemistry of the sediments indicated that the dominant elemental oxide was $ SiO_{2} $ followed by $ Al_{2} %$ O_{3} $ in all the sediments. The Chemical Index Alteration (CIA) and Resistant Index of Maturity ($ R_{M} $) reflected moderate weathering and immaturity of the sediments in the basin. Grain size (dpeaa)DE-He213 Weathering (dpeaa)DE-He213 Jhelum (dpeaa)DE-He213 Kashmir valley (dpeaa)DE-He213 Himalaya (dpeaa)DE-He213 Jeelani, Gh aut Enthalten in Journal of the Geological Society of India New Delhi : Springer India, 1959 86(2015), 4 vom: Okt., Seite 445-458 (DE-627)60666078X (DE-600)2508930-4 0974-6889 nnns volume:86 year:2015 number:4 month:10 pages:445-458 https://dx.doi.org/10.1007/s12594-015-0332-2 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 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_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 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_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 86 2015 4 10 445-458 |
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10.1007/s12594-015-0332-2 doi (DE-627)SPR02621265X (SPR)s12594-015-0332-2-e DE-627 ger DE-627 rakwb eng Mir, Riyaz Ahmad verfasserin aut Textural characteristics of sediments and weathering in the Jhelum river basin located in Kashmir Valley, Western Himalaya 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Geological Society of India 2015 Abstract This study presents a detailed textural and geochemical study of sediments of river Jhelum and its tributaries of Kashmir valley. The textural studies clearly established that the sediments were dominantly of medium grain size, moderately sorted and very positively skewed. The kurtosis suggested dominantly leptokurtic nature of sediments. The sediments were deposited under moderate to low energy conditions with dominant rolling processes. The statistical parameters showed little spatial as well as temporal variations. The observations are supported by the frequency curves and bivariate plots between various textural parameters, confirming the polymodal nature of sediments with dominant to moderate sand fraction. The bimodal and unimodal nature of the sediments was also present at certain locations. The major oxide elemental chemistry of the sediments indicated that the dominant elemental oxide was $ SiO_{2} $ followed by $ Al_{2} %$ O_{3} $ in all the sediments. The Chemical Index Alteration (CIA) and Resistant Index of Maturity ($ R_{M} $) reflected moderate weathering and immaturity of the sediments in the basin. Grain size (dpeaa)DE-He213 Weathering (dpeaa)DE-He213 Jhelum (dpeaa)DE-He213 Kashmir valley (dpeaa)DE-He213 Himalaya (dpeaa)DE-He213 Jeelani, Gh aut Enthalten in Journal of the Geological Society of India New Delhi : Springer India, 1959 86(2015), 4 vom: Okt., Seite 445-458 (DE-627)60666078X (DE-600)2508930-4 0974-6889 nnns volume:86 year:2015 number:4 month:10 pages:445-458 https://dx.doi.org/10.1007/s12594-015-0332-2 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 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_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 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_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 86 2015 4 10 445-458 |
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Mir, Riyaz Ahmad |
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Mir, Riyaz Ahmad misc Grain size misc Weathering misc Jhelum misc Kashmir valley misc Himalaya Textural characteristics of sediments and weathering in the Jhelum river basin located in Kashmir Valley, Western Himalaya |
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Textural characteristics of sediments and weathering in the Jhelum river basin located in Kashmir Valley, Western Himalaya Grain size (dpeaa)DE-He213 Weathering (dpeaa)DE-He213 Jhelum (dpeaa)DE-He213 Kashmir valley (dpeaa)DE-He213 Himalaya (dpeaa)DE-He213 |
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textural characteristics of sediments and weathering in the jhelum river basin located in kashmir valley, western himalaya |
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Textural characteristics of sediments and weathering in the Jhelum river basin located in Kashmir Valley, Western Himalaya |
| abstract |
Abstract This study presents a detailed textural and geochemical study of sediments of river Jhelum and its tributaries of Kashmir valley. The textural studies clearly established that the sediments were dominantly of medium grain size, moderately sorted and very positively skewed. The kurtosis suggested dominantly leptokurtic nature of sediments. The sediments were deposited under moderate to low energy conditions with dominant rolling processes. The statistical parameters showed little spatial as well as temporal variations. The observations are supported by the frequency curves and bivariate plots between various textural parameters, confirming the polymodal nature of sediments with dominant to moderate sand fraction. The bimodal and unimodal nature of the sediments was also present at certain locations. The major oxide elemental chemistry of the sediments indicated that the dominant elemental oxide was $ SiO_{2} $ followed by $ Al_{2} %$ O_{3} $ in all the sediments. The Chemical Index Alteration (CIA) and Resistant Index of Maturity ($ R_{M} $) reflected moderate weathering and immaturity of the sediments in the basin. © Geological Society of India 2015 |
| abstractGer |
Abstract This study presents a detailed textural and geochemical study of sediments of river Jhelum and its tributaries of Kashmir valley. The textural studies clearly established that the sediments were dominantly of medium grain size, moderately sorted and very positively skewed. The kurtosis suggested dominantly leptokurtic nature of sediments. The sediments were deposited under moderate to low energy conditions with dominant rolling processes. The statistical parameters showed little spatial as well as temporal variations. The observations are supported by the frequency curves and bivariate plots between various textural parameters, confirming the polymodal nature of sediments with dominant to moderate sand fraction. The bimodal and unimodal nature of the sediments was also present at certain locations. The major oxide elemental chemistry of the sediments indicated that the dominant elemental oxide was $ SiO_{2} $ followed by $ Al_{2} %$ O_{3} $ in all the sediments. The Chemical Index Alteration (CIA) and Resistant Index of Maturity ($ R_{M} $) reflected moderate weathering and immaturity of the sediments in the basin. © Geological Society of India 2015 |
| abstract_unstemmed |
Abstract This study presents a detailed textural and geochemical study of sediments of river Jhelum and its tributaries of Kashmir valley. The textural studies clearly established that the sediments were dominantly of medium grain size, moderately sorted and very positively skewed. The kurtosis suggested dominantly leptokurtic nature of sediments. The sediments were deposited under moderate to low energy conditions with dominant rolling processes. The statistical parameters showed little spatial as well as temporal variations. The observations are supported by the frequency curves and bivariate plots between various textural parameters, confirming the polymodal nature of sediments with dominant to moderate sand fraction. The bimodal and unimodal nature of the sediments was also present at certain locations. The major oxide elemental chemistry of the sediments indicated that the dominant elemental oxide was $ SiO_{2} $ followed by $ Al_{2} %$ O_{3} $ in all the sediments. The Chemical Index Alteration (CIA) and Resistant Index of Maturity ($ R_{M} $) reflected moderate weathering and immaturity of the sediments in the basin. © Geological Society of India 2015 |
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Textural characteristics of sediments and weathering in the Jhelum river basin located in Kashmir Valley, Western Himalaya |
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https://dx.doi.org/10.1007/s12594-015-0332-2 |
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Jeelani, Gh |
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10.1007/s12594-015-0332-2 |
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