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Kothare, Prajakta
- A Note on Inch Scale Layering in a Dolerite Dyke of the Deccan Trap of Saurashtra, India
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Authors
Affiliations
1 Department of Geology, St. Xavier's College, Mumbai - 400 001, IN
1 Department of Geology, St. Xavier's College, Mumbai - 400 001, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 54, No 2 (1999), Pagination: 187-192Abstract
Distinct vertical rhythmic layering is seen in one of the dykes 68 km southeast of Rajkot. The dyke extends for almost 50 km in length but has a limited width of 10 to 15 metres. The vertical layering is due to alternating layers rich in plagioclase and pyroxene, which is encountered mainly in the central part of the dyke. The layering is formed due to molecuIar diffusion at the front of cooling and crystallization with the temperature gradient catching up gradually to form the next layer. Alternatively it may be possible that layering is due to multiple injections of melt into the fracture that was responsible for disturbing the equilibrium from time to time.Keywords
Petrology, Deccan Trap, Olivine Dolerite Dyke, Layering, Saurashtra.- Geology and Petrography of the Intrusives in the Deccan Trap of Central and South-Eastern Saurashtra, India
Abstract Views :176 |
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Authors
Affiliations
1 Department of Geology, St. Xavier's College, Mumbai - 400 001, IN
1 Department of Geology, St. Xavier's College, Mumbai - 400 001, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 57, No 3 (2001), Pagination: 249-256Abstract
Forty-five major dykes intruding the Deccan Trap were studied in the central and south-eastern parts of Saurashtra. There are some distinct structural differences seen between the area north of Amreli and that south of Amreli. The lava flows north of Amreli are practically horizontal, while south of Amreli they seem to be forming a major southerly-plunging antiform. In the area north of Amreli, dolerite dykes are invariably enriched in fresh olivine and are associated with one ankaramite dyke, a hybrid monzodolerite and a stock-like body of essexite (foid monzogabbro). In the area south of Armeli, dolerites are generally olivine free but in a few samples altered olivine is present. These dolerites are associated with rhyolitic dykes, which invariably contain microphenocrysts of quartz and are thus described as quartz porphyries.Keywords
Deccan Trap, Intrusives, Petrography, Structure, Saurashtra.- Petrology and Mineralogy of Ankaramite in the Deccan Volcanic Province of Rajkot District, Saurashtra, Gujarat
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Authors
Affiliations
1 Department of Geology, St. Xavier's College, Mumbai - 400 001, IN
1 Department of Geology, St. Xavier's College, Mumbai - 400 001, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 61, No 1 (2003), Pagination: 97-100Abstract
The occurrence of ankaramite in the Deccan Volcanic Province of Saurashtra is reported here. The ankaramite occurs as a small dyke intruding into horizontal basalt flows. Petrographically it is characterised by the presence of large phenocrysts of ctinopyroxene (chromian diopside) and olivine (Fo83) in a groundmass of plagioclase (An60), iron oxides and accessory brown amphibole (kaersutite). Chemically it is characterised by enrichment in high field strength and light rare earth elements as compared to the picritic olivine dolerites of the area. It is concluded that the ankaramite magma represents a primitive sample of High-Ti type of tholeiitic basaltic magma while majority of the olivine dolerites and dolerites found in the area are representative of Low-Ti type of tholeiitic magma.Keywords
Deccan Traps, Ankaramite, Rajkot, Saurashtra, Gujarat.- Monzodolerite Dyke in the Deccan Traps of Saurashtra
Abstract Views :172 |
PDF Views:3
Authors
Affiliations
1 Department of Geology, St. Xavier's College, Mumbai - 400 001, IN
1 Department of Geology, St. Xavier's College, Mumbai - 400 001, IN