Magmatic processes leading to compositional diversity in igneous rocks: Bowen (1928) revisited

2018 ◽  
Vol 318 (1) ◽  
pp. 1-28 ◽  
Author(s):  
Timothy L. Grove ◽  
Stephanie M. Brown
Keyword(s):  
Igneous Rocks ◽  
Magmatic Processes ◽  
Compositional Diversity

scholarly journals Editorial for the Special Issue “Mineral Textural and Compositional Variations as a Tool for Understanding Magmatic Processes”

Minerals ◽  
2021 ◽  
Vol 11 (2) ◽  
pp. 102
Author(s):  
Silvio Mollo ◽  
Flavio Di Stefano ◽  
Francesca Forni
Keyword(s):  
Magma Chamber ◽  
Igneous Rocks ◽  
Eruption Dynamics ◽  
Special Issue ◽  
Magma Chamber Processes ◽  
Magmatic Processes ◽  
Compositional Variations

This Special Issue of Minerals collects seven different scientific contributions highlighting how magma chamber processes and eruption dynamics studied either in the laboratory or in nature may ultimately control the evolutionary histories and geochemical complexities of igneous rocks [...]

Sm–Nd isotopic investigation of Neoproterozoic and Cretaceous igneous rocks from southern Brazil: A study of magmatic processes

Lithos ◽  
2005 ◽  
Vol 82 (3-4) ◽  
pp. 345-377 ◽  
Author(s):  
Maria do Carmo P. Gastal ◽  
Jean Michel Lafon ◽  
Léo Afraneo Hartmann ◽  
Edinei Koester
Keyword(s):  
Igneous Rocks ◽  
Southern Brazil ◽  
Magmatic Processes ◽  
Isotopic Investigation

Beyond compositional diversity: Examining the campus climate experiences of Asian American and Pacific Islander students.

2018 ◽  
Vol 11 (4) ◽  
pp. 484-501 ◽  
Author(s):  
Mike Hoa Nguyen ◽  
Jason Chan ◽  
Bach Mai Dolly Nguyen ◽  
Robert T. Teranishi
Keyword(s):  
Asian American ◽  
Campus Climate ◽  
Pacific Islander ◽  
Compositional Diversity

Geological study in Tal - Talekhu section of Manang District along the Besisahar – Chame Road

2020 ◽  
Vol 22 ◽  
pp. 25-28
Author(s):  
Prakash Luitel ◽  
Suman Panthee
Keyword(s):  
Cross Section ◽  
Geological Mapping ◽  
Igneous Rocks ◽  
Geological Cross Section ◽  
Lowermost Part ◽  
Migmatitic Gneiss

The section between Tal to Talekhu of Manang District lacks the detailed geological study. The geological mapping in the scale of 1:50,000 followed by the preparation of geological cross-section and lithostratigraphic column has been done in the present study. The studied area lies partially in the Higher Himalayan Crystalline and the Tibetan Tethys Sequence. The units of the Higher Himalayan Group from Tal to Talekhu consists mainly of vigorous to faintly calcareous gneiss, migmatitic gneiss, quartzite, granite, etc. They are named as the Calc. Silicate Gneiss and Paragneiss and the Orthogneiss and Granite units. The lowermost part of the Tibetan Tethys consisted of metamorphosed calcareous rocks containing silicates and feldspar, so this unit is termed as the Marble and Calc. Gneiss. The section is about 9 km in thickness and is highly deformed with presence of igneous rocks at many places.

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