Zobrazeno 1 - 10
of 10
pro vyhledávání: '"Shabber H. Alvi"'
Autor:
Shabber H. Alvi, Mohd. Shaif
Publikováno v:
Geology, Ecology, and Landscapes, Vol 5, Iss 4, Pp 260-268 (2021)
Palaeoproterozoic Noamundi – Koira Basin (NKB), on the western margin of the >3.0 Ga old Singhbhum Granitoid Complex, forms a horseshoe-shaped synclinorium. Volcanic rocks belonging to Bonai volcanic suite (BVS) occur outside and all-around the NKB
Externí odkaz:
https://doaj.org/article/0aef44cd415f4ce4ae79def30d6e8ccb
Autor:
Shabber H. Alvi, Usman Aarif Chaudhary
Publikováno v:
Journal of the Geological Society of India. 97:315-325
Singhbhum craton preserves the records of sedimentation, magmatism, and tectono-thermal events from Mesoarchaean to Neoproterozoic. The Dhanjori Group (DG), located on the northeast margin of the Singhbhum craton, comprises of a variety of rocks incl
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::faa8de4474a5c76f3910025952837c14
https://doi.org/10.1007/s12594-021-1683-5
https://doi.org/10.1007/s12594-021-1683-5
Publikováno v:
Journal of the Geological Society of India. 94:351-358
The Dalma metavolcanic belt is composed of ultramafics at the base, tuffs on top and basalts in-between. It extends for about 200kms east-west in the middle of the Proterozoic Singhbhum Mobile Belt. Ultramafics are chiefly composed of actinolite, hor
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::dee908d57084132828c4a220dd60f710
https://doi.org/10.1007/s12594-019-1322-6
https://doi.org/10.1007/s12594-019-1322-6
Physico-Chemical Analysis of Groundwater in Iglas and Beswan, Aligarh District, Uttar Pradesh, India
Publikováno v:
Latest Advancements in Underground Structures and Geological Engineering ISBN: 9783030341770
Iglas and Beswan are the towns in Aligarh district in of Uttar Pradesh, India. These are located along Aligarh- Mathura high way at 24 km from Aligarh. These are located at 27°43′ N 77°56′ E. It has an average elevation of 178 m. The town area
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ce8d193757ee7a40106094fd88e2db82
https://doi.org/10.1007/978-3-030-34178-7_9
https://doi.org/10.1007/978-3-030-34178-7_9
Autor:
Usman Aarif Chaudhary, Mahmoud A. Galmed, Bassam A. Abuamarah, Naurin Khan Malik, Shabber H. Alvi
Publikováno v:
Journal of King Saud University: Science, Vol 33, Iss 1, Pp 101264-(2021)
Paleoproterozoic mobile belt of Eastern India well known as Singhbhum Mobile Belt (SMB) bears the evidences of tectono-magmatic processes and crustal evolution like many other major Precambrian terrains of the world. Because of some significant major
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::515de3928f075ba9f741fdbd7acfb28c
https://doi.org/10.1016/j.jksus.2020.101264
https://doi.org/10.1016/j.jksus.2020.101264
Publikováno v:
Chinese Journal of Geochemistry. 34:241-251
The high-Mg mafic dykes from the Singhbhum Granitoid Complex in East India have geochemical characteristics [e.g., enrichment of the large ion lithophile elements and light rare earth elements (LREEs) relative to high field strength elements (HFSEs):
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::023387f16c5fbacc0af59776caa658c2
https://doi.org/10.1007/s11631-015-0044-8
https://doi.org/10.1007/s11631-015-0044-8
Publikováno v:
Arabian Journal of Geosciences. 4:933-943
Singhbhum granitoid complex has been intruded by numerous mafic dykes trending in different directions. The studied dykes were originated from subalkaline magma, ranging in composition from basalt through basaltic-andesite to andesite. In the present
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::56dc0d8fba515037c5c178f342e2ed5f
https://doi.org/10.1007/s12517-010-0121-6
https://doi.org/10.1007/s12517-010-0121-6
Publikováno v:
International Geology Review. 52:79-94
Mafic dikes, which transect the Mesoarchaean Singhbhum Granitoid Complex, are the most abundant members of the Newer Dolerite dikes of the Singhbhum Orissa craton. These dikes are subalkaline and exhibit a tholeiitic differentiation trend. Studied di
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f7ac46c46d2e778ae49bf921ec5071be
https://doi.org/10.1080/00206810903211948
https://doi.org/10.1080/00206810903211948
Publikováno v:
International Geology Review. 53:46-60
The Singhbhum Orissa craton, eastern India contains rocks as old as 3.6 Ga. The Newer Dolerites occur in two distinct orientations (NE/SW and NW/SE) in the Singhbhum Granitoid Complex (SBGC). These dikes are mostly tholeiites and quartz-normative dol
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8a8d5b5d157247e5c861500126ae8a59
https://doi.org/10.1080/00206810902900053
https://doi.org/10.1080/00206810902900053
Autor:
M. Raza, Shabber H. Alvi
Publikováno v:
Geological Magazine. 129:337-348
Geochemical data on the Dhanjori volcanics of the Singhbhum craton indicate that they range from basalt to andesite and show an iron-enrichment trend. Various chemical characteristics suggest that they are differentiated along the trend similar to th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6c296e0f69c20c002c267dac4cd22e7b
https://doi.org/10.1017/s0016756800019270
https://doi.org/10.1017/s0016756800019270