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Sinha, K. K.
- Need Based Trainings and Constraints of Banana Growers in Bhagalpur, Bihar
Abstract Views :224 |
PDF Views:0
Authors
Affiliations
1 Department of Extension Education, Bihar Agricultural University, Bangalpur Bihar, IN
2 Department of Extension Education, Rajendra Agricultural University, Samstipur Bihar, IN
3 Department of Plant Pathology, Bihar Agricultural University, Bangalpur Bihar, IN
1 Department of Extension Education, Bihar Agricultural University, Bangalpur Bihar, IN
2 Department of Extension Education, Rajendra Agricultural University, Samstipur Bihar, IN
3 Department of Plant Pathology, Bihar Agricultural University, Bangalpur Bihar, IN
Source
Agriculture Update, Vol 8, No 3 (2013), Pagination: 509-513Abstract
No AbstractKeywords
Training, Constrains, Banana Growers
- Constraints Faced by the Wheat Growers in Adoption of Wheat Production Technology
Abstract Views :300 |
PDF Views:0
Authors
A. K. Paswan
1,
K. K. Sinha
2
Affiliations
1 Department of Extension Education, Tirhut College of Agriculture, Dholi,Muzaffarpur Bihar, IN
2 Department of Extension Education, Rajendra Agricultural University, Pusa, Samastipur Bihar, IN
1 Department of Extension Education, Tirhut College of Agriculture, Dholi,Muzaffarpur Bihar, IN
2 Department of Extension Education, Rajendra Agricultural University, Pusa, Samastipur Bihar, IN
Source
Agriculture Update, Vol 9, No 2 (2014), Pagination: 166-169Abstract
The study was conducted to find out constraints faced by wheat growers in adoption of wheat production technology. The constraints which were most perceived by the wheat growers were non-availability of production inputs at village level, lack of easily available credits, fragmentation of land holding, lack of soil testing facilities at nearby place and high cost of diesel.Keywords
Constraints, Adoption, Production Technology- Timmasamudram Kimberlite Cluster, Wajrakarur Kimberlite Field, Anantapur District, Andhra Pradesh
Abstract Views :200 |
PDF Views:2
Authors
Affiliations
1 Project: Diamond, OP: Andhra Pradesh, Geological Survey of India, Southern Region, Hyderabad – 500 068, IN
1 Project: Diamond, OP: Andhra Pradesh, Geological Survey of India, Southern Region, Hyderabad – 500 068, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 69, No Spl Iss 3 (2007), Pagination: 597-609Abstract
A cluster of four kimberlite bodies was discovered on the left bank of the Penner River near Timmasamudram village. Falling in the area known for alluvial diamond occurrences within the Wajrakarur Kimberlite Field (WKF), this cluster is located between the Kalyandurg Kimberlite Cluster in the west and Chigicherla Kimberlite cluster in the east. With the addition of kimberlite bodies in the present cluster, christened as the Timmasamudram Kimberlite Cluster (TKC), the total number of kimberlite bodies in WKF reaches to 27. Texturally, mineralogically and chemically, the kimberlite bodies in TKC match with the archetypal Group-I kimberlites. Typically they fall in the non-micaceous kimberlite field. The mantle xenocrystic mineral chemistry shows conditions congenial for diamond formation in these pipes, which is further supported by actual microdiamond recovery from the soft kimberlitic yellow ground.Keywords
Kimberlite, Timmasamudram Kimberlite Cluster, Group-I kimberlites, Microdiamonds, Andhra Pradesh.- Mineralogical and Geochemical Characteristics of the Basal Quartz - Pebble Conglomerate of Dhanjori Group, Singhbhum Craton, India and their Significance
Abstract Views :243 |
PDF Views:3
Authors
T. S. Sunil Kumar
1,
N. Krishna Rao
1,
M. M. Palrecha
2,
R. Parthasarathy
2,
V. L. Shah
3,
K. K. Sinha
4
Affiliations
1 Ore Dressing Section, Bhabha Atomic Research Centre, Hyderabad 500 016, IN
2 Analytical Chemistry Division, Bhabha Atomic Research Centre, Mumbai 400 085, IN
3 Atomic Minerals Division, Begumpet, Hyderabad 500 016, IN
4 Prem Mandir, Anugrah Narayan Road, Kadamkuan, Patna 800 003, IN
1 Ore Dressing Section, Bhabha Atomic Research Centre, Hyderabad 500 016, IN
2 Analytical Chemistry Division, Bhabha Atomic Research Centre, Mumbai 400 085, IN
3 Atomic Minerals Division, Begumpet, Hyderabad 500 016, IN
4 Prem Mandir, Anugrah Narayan Road, Kadamkuan, Patna 800 003, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 51, No 6 (1998), Pagination: 761-776Abstract
he basal quartz-pebble conglomerate of Dhanjori Group of Singhbhum-Orissa craton is characterised by a distinct heavy mineral assemblage of pink zircon, chromite, pyrite, monazite and rutile-silicate intergrowth. Statistical analysis of morphometric features of zircons shows that they are significantly different from those found in Older Metamorphic Group and Older Metamorphic Tonalite Gneiss, but they have resemblance to those found in Singhbhum Granite. The trace and REE characteristics of the conglomerates, and the morphology and chemistry of zircon, identify the Singhbhum Granite Complex as the predominant source rock. At the same time, abundant detrital chromite, the positive trend of Cr-Ni and Cr-Co plots, and high Cr/Th ratios of the QPCs suggest a mixed provenance with an ultramafic component ofkomatiitic affinity (older greenstones) in the granite complex. The relative proportion of older greenstones was higher towards western and southern margins of the Dhanjori basin.Keywords
Mineralogy, Geochemistry, Quartz-Pebble Conglomerate, Dhanjori Group, Singhbhum-Orissa Craton.- A Note on Petrography and Chemistry of Microgranular Enclaves and Granitoids around Talbahat, Lalitpur District, Uttar Pradesh
Abstract Views :191 |
PDF Views:160
Authors
Affiliations
1 Atomic Minerals Directorate for Exploration and Research, Begumpet, Hyderabad - 500 016, IN
2 Atomic Minerals Directorate for Exploration and Research, Nongmynsong, PO Assam Rifles, Shillong-793 001, IN
1 Atomic Minerals Directorate for Exploration and Research, Begumpet, Hyderabad - 500 016, IN
2 Atomic Minerals Directorate for Exploration and Research, Nongmynsong, PO Assam Rifles, Shillong-793 001, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 65, No 1 (2005), Pagination: 92-96Abstract
No Abstract.Full Text
- Peperite Occurrence and its Implications on Origin and Temporal Development of the Proterozoic Dhala Basin, Mohar Area, Shivpuri District, Madhya Pradesh
Abstract Views :190 |
PDF Views:0
Authors
Affiliations
1 Atomic Minerals Directorate for Exploration and Research, West Block VII, R.K. Puram, New Delhi - 110 067, IN
2 Atomic Minerals Directorate for Exploration and Research, AMD Complex, 1-10-153/156, Begumpet, Hyderabad - 500 016, IN
1 Atomic Minerals Directorate for Exploration and Research, West Block VII, R.K. Puram, New Delhi - 110 067, IN
2 Atomic Minerals Directorate for Exploration and Research, AMD Complex, 1-10-153/156, Begumpet, Hyderabad - 500 016, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 77, No 2 (2011), Pagination: 183-189Abstract
In the western part of Bundelkhand massif, a caldera with intra-caldera sediments, known as Dhala Formation, occurs as an outlier in and around Mohar village of Shivpuri district, Madhya Pradesh. For the first time, occurrence of peperite is being reported from the basal part of the Dhala sediment. Two types of peperites have been recognized: blocky and fluidal or globular with variable morphology. In peperitic zones, features like soft sediment deformations, presence of sediment into the rhyolite along cracks, vesiculation of the sediments and other evidences suggestive of sediment fluidization are some definite characteristics of interaction of hot magma with wet sediments forming peperite. The occurrence of peperites reflects the contemporaniety of deposition of the Dhala sediments and volcanism, which is well in accordance to the volcanic origin of Dhala structure. Further, the nature of unconformity between the Dhala and overlying Kaimur which is characterized by merely a few centimeter thick pebbly/conglomeratic bed does not appear to represent a large hiatus as expected between the Semri and Kaimur of Vindhyan Supergroup. So, the contemporaniety of the Dhala Formation (at least the lower part) as reflected by occurrence of peperites, coupled with the available age of the rhyolite and the nature of the unconformity between the Dhala and overlying Kaimur provide convincing evidence to correlate the Dhala Formation with the Lower part of the Kaimur and unlikely with the Semri Group or Bijawar as proposed earlier.Keywords
Caldera, Peperites, Dhala Sediment, Bundelkhand, Vindhyans, Madhya Pradesh.- Stratigraphic Succession of Precambrian of Singhbhum: Evidence from Quartz Pebble Conglomerate
Abstract Views :262 |
PDF Views:2
Authors
Affiliations
1 Prem Mandir, Anugrah Narayan Road, Kadamkuan, Patna - 800 003, IN
2 Ore Dressing Section, Bhabha Atomic Research Centre, Hyderabad - 500 016, IN
3 Atomic Minerals Division, Begumpet, Hyderabad - 500 016, IN
1 Prem Mandir, Anugrah Narayan Road, Kadamkuan, Patna - 800 003, IN
2 Ore Dressing Section, Bhabha Atomic Research Centre, Hyderabad - 500 016, IN
3 Atomic Minerals Division, Begumpet, Hyderabad - 500 016, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 49, No 5 (1997), Pagination: 577-588Abstract
Though the stratigraphic succession in the Precambrian of Singbhum-Orissa region of the Indian shield given by Saba et al. is widely accepted, there are several contentious issues whieh have been hotly debated over the years. The occurrence of uraninite and pyrite bearing quartz-pebble conglomerate at the base of Iron Ore Group (lOG) as well as the Dhanjori Group has indicated the necessity for a revision in the stratigraphic succession in view of the temporal significance of such conglomerate the world over.
The conglomerate contains a significant population of zircon, chromite and shows a typical minor and trace element composition. The zircon has morphometric properties similar to those found in several members of the Singhbhum Granite Complex. The presence of detrital chromite and high Cr content indicate the occurrence of older mafics/ultramafics in the provenance along with the Singhbhum Granite Complex. It is suggested that some mafic and ultramafic members presently grouped within the IOG may represent such "older greenstones". The IOG as well as the Dhanjori Group with basal QPC horizon lie over a basement of Singhbhum Granite-Greenstone Complex. From available evidences it is surmised that both IOG sensu stricto (the BIF sequence and associated ferruginous cherts. greywackes and acid-intennediate volcanics) and the Dhanjori Group represent late Archaean (2500-3000 Ma) supracrustals and hence are nearly coeval. The Singhbhum Group north of the shear zone represents early Proterozoic supracrustals.