Mineralogy and petrology of lamprophyre and dolerite dykes from the end-Cretaceous (~ 66 Ma) Phenaimata alkaline igneous complex, north-western India: evidence for open magma chamber fractionation, mafic recharge, and disaggregation of crystal mush zone in a large igneous province-Reference-Cited by-同舟云学术

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Mineralogy and petrology of lamprophyre and dolerite dykes from the end-Cretaceous (~ 66 Ma) Phenaimata alkaline igneous complex, north-western India: evidence for open magma chamber fractionation, mafic recharge, and disaggregation of crystal mush zone in a large igneous province

Published:2021-11-15 Issue: Volume: Page:
ISSN:0930-0708
Container-title:Mineralogy and Petrology
language:en
Short-container-title:Miner Petrol

Author:

Sharma Abhinay,Pandey Rohit,Rao Nittala V. Chalapathi^ORCID,Sahoo Samarendra,Belyatsky Boris V.,Dhote Prashant

Funder

Science and Engineering Research Board

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

https://link.springer.com/content/pdf/10.1007/s00710-021-00770-y.pdf

Reference100 articles.

1. Adam J, Green T (2006) Trace element partitioning between mica-and amphibole-bearing garnet lherzolite and hydrous basanitic melt: 1. Experimental results and the investigation of controls on partitioning behaviour. Contrib Mineral Petrol 152(1):117.https://doi.org/10.1007/s00410-006-0085-4

2. Adam J, Green TH (1994) The effects of pressure and temperature on the partitioning of Ti, Sr and REE between amphibole, clinopyroxene and basanitic melts. Chem Geol 117(1–4):219–233. https://doi.org/10.1016/0009-2541(94)90129-5

3. Akinin VV, Sobolev AV, Ntaflos T, Richter W (2005) Clinopyroxene megacrysts from Enmelen melanephelinitic volcanoes (Chukchi Peninsula, Russia): application to composition and evolution of mantle melts. Contrib Mineral Petrol 150(1):85–101. https://doi.org/10.1007/s00410-005-0007-x

4. Ashwal LD, Ziegler A, Glynn S, Truebody T, Bolhar R (2021) Sr‐enriched glassy picrites from the Karoo Large Igneous Province are evolved, not primitive magmatic rocks. Geochem Geophysi Geosyst 22(4), p.e2020GC009561. https://doi.org/10.1029/2020GC009561

5. Bachmann O, Bergantz GW (2008) Rhyolites and their source mushes across tectonic settings. J Petrol 49(12):2277–2285

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1. Mineral chemistry of chrome-diopside bearing lamprophyre from Mesoproterozoic Settupalle igneous complex of Prakasam alkaline province: insights on the magma dynamics at shallow lithospheric mantle beneath the NE margin of the Cuddapah basin, Southern India;Geological Society, London, Special Publications;2024-07-09

2. Petrology, mineral chemistry and geochemistry of lamprophyres from Rongjeng–Nongchram area, East Garo Hills, Shillong Plateau, Meghalaya, Northeast India;Journal of Earth System Science;2024-01-11

3. Heterogeneous mush-dominated plumbing system and mantle sources of alkaline lamprophyres in Tuoyun Basin, SW Central Asian Orogenic Belt;Geological Society of America Bulletin;2023-09-08

4. Alkaline rocks from the Deccan Large Igneous Province: Time–space distribution, petrology, geochemistry and economic aspects;Journal of Earth System Science;2022-04-30

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