Geochemistry and petrogenesis of Proterozoic mafic rocks from East Khasi Hills, Shillong Plateau, Northeastern India

2013 ◽  
Vol 230 ◽  
pp. 119-137 ◽  
Author(s):  
Jyotisankar Ray ◽  
Abhishek Saha ◽  
Christian Koeberl ◽  
Martin Thoni ◽  
Sohini Ganguly ◽  
...  
2011 ◽  
Vol 20 (2-3) ◽  
pp. 395-404 ◽  
Author(s):  
Md. Shofiqul Islam ◽  
Ryuichi Shinjo ◽  
J.R. Kayal

Author(s):  
Alasdair Skelton ◽  
Lillemor Claesson ◽  
Govinda Chakrapani ◽  
Chandan Mahanta ◽  
Joyanto Routh ◽  
...  

2008 ◽  
Vol 165 (1) ◽  
pp. 45-61 ◽  
Author(s):  
Alasdair Skelton ◽  
Lillemor Claesson ◽  
Govinda Chakrapani ◽  
Chandan Mahanta ◽  
Joyanto Routh ◽  
...  

2012 ◽  
Vol 76 (5) ◽  
pp. 1099-1117 ◽  
Author(s):  
L. Melluso ◽  
R. K. Srivastava ◽  
C. M. Petrone ◽  
V. Guarino ◽  
A. K. Sinha

AbstractThe rocks of the Jasra intrusive complex (Shillong Plateau, northeastern India) include phlogopite clinopyroxenites (with olivine or perovskite relics), alkali gabbros/monzodiorites, syenites and nepheline syenites. They have a potassic affinity (Na2O/K2O ∼1), and their mineralogy is dominated by clinopyroxene with which phlogopite, olivine, amphibole, feldspars, feldspathoids, oxides, orthopyroxenes, perovskite, titanite and other accessory phases are variably associated. The Jasra intrusive rocks are cumulates derived from at least two distinct magmatic liquids. The potassic affinity of the Jasra rocks differs from the nearby Sung Valley ijolitic-carbonatitic complex and from the ultrapotassic lamproitic rocks of the Damodar Valley, which are of approximately the same age. This suggests major variability in the mantle sources of small-volume alkaline volcanism in the Early Cretaceous of northeastern India.


2015 ◽  
Vol 124 (2) ◽  
pp. 459-475 ◽  
Author(s):  
Sampa Hazra ◽  
Jyotisankar Ray ◽  
C Manikyamba ◽  
Abhishek Saha ◽  
S S Sawant

2009 ◽  
Vol 22 (3) ◽  
pp. 283-291 ◽  
Author(s):  
Saurabh Baruah ◽  
Santanu Baruah ◽  
Naba Kumar Gogoi ◽  
Olga Erteleva ◽  
Felix Aptikaev ◽  
...  

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