Chronological and Geochemical Study on Cenozoic Potassic Felsic Igneous Rocks in Western Yunnan, SE Tibet: Implications for their Tectonic Mechanisms

2021 ◽  
Author(s):  
WanLi TANG ◽  
JianLin CHEN ◽  
Rongyu TAN
Keyword(s):  
Igneous Rocks ◽  
Geochemical Study ◽  
Western Yunnan ◽  
Se Tibet

Petrogenesis of the mafic igneous rocks of the Betic Cordilleras: A field, petrological and geochemical study

2000 ◽  
Vol 139 (4) ◽  
pp. 436-457 ◽  
Author(s):  
Maria Teresa Gómez-Pugnaire ◽  
Peter Ulmer ◽  
Vicente López-Sánchez-Vizcaíno
Keyword(s):  
Igneous Rocks ◽  
Betic Cordilleras ◽  
Geochemical Study

scholarly journals The chemistry and petrogenesis of igneous rocks of the Karoo central area, southern Africa. 1984. Kraai River Pass.xls

2020 ◽  
Author(s):  
Hugh V Eales
Keyword(s):  
Major Element ◽  
Central Area ◽  
Igneous Rocks ◽  
Lava Flows ◽  
Primary Sources ◽  
Eastern Cape ◽  
Original Source ◽  
Geochemical Study ◽  
North Eastern ◽  
Area North

<p>Analyses in this dataset are from the following primary sources:</p> <p>Bowen, MP (1979) Some petrological aspects of the Omega Member flow unit, Barkly East District. Unpublished BSc Honours project, Rhodes University, 83pp.</p> <p>Pemberton, M (1979) A study of the massive unit of the Omega Member near Barkly East. Unpublished BSc Honours project, Rhodes University, 44pp</p> <p>Minne, HFD (1975) A study of a sequence of lava flows in the lower part of the Drakensberg Subgroup near Barkly East. Unpublished BSC Honours project, Rhodes University, 38pp</p> <p>Pemberton, J (1978) The geochemistry and petrology of Karoo basalts of the Barkly East area, north-eastern Cape. Unpublished MSc thesis, Rhodes University, 139pp</p> <p>Barrie, PD (1977) The Kraai River Formation: a petrographical and geochemical study of an occurrence in the vicinity of Barkly East. Unpublished BSC Honours project, Rhodes University.</p> <p>Major element analyses from original source. All trace elements redetermined in 2004.</p>

scholarly journals The chemistry and petrogenesis of igneous rocks of the Karoo central area, southern Africa. 1984. Kraai River Pass.xls

2020 ◽  
Author(s):  
Hugh V Eales ◽  
Julian S Marsh
Keyword(s):  
Major Element ◽  
Central Area ◽  
Igneous Rocks ◽  
Lava Flows ◽  
Primary Sources ◽  
Eastern Cape ◽  
Original Source ◽  
Geochemical Study ◽  
North Eastern ◽  
Area North

<p>Analyses in this dataset are from the following primary sources:</p> <p>Bowen, MP (1979) Some petrological aspects of the Omega Member flow unit, Barkly East District. Unpublished BSc Honours project, Rhodes University, 83pp.</p> <p>Pemberton, M (1979) A study of the massive unit of the Omega Member near Barkly East. Unpublished BSc Honours project, Rhodes University, 44pp</p> <p>Minne, HFD (1975) A study of a sequence of lava flows in the lower part of the Drakensberg Subgroup near Barkly East. Unpublished BSC Honours project, Rhodes University, 38pp</p> <p>Pemberton, J (1978) The geochemistry and petrology of Karoo basalts of the Barkly East area, north-eastern Cape. Unpublished MSc thesis, Rhodes University, 139pp</p> <p>Barrie, PD (1977) The Kraai River Formation: a petrographical and geochemical study of an occurrence in the vicinity of Barkly East. Unpublished BSC Honours project, Rhodes University.</p> <p>Major element analyses from original source. All trace elements redetermined in 2004.</p>

scholarly journals The chemistry and petrogenesis of igneous rocks of the Karoo central area, southern Africa. 1984. Kraai River Pass.xls

2020 ◽  
Author(s):  
Hugh V Eales ◽  
Julian S Marsh
Keyword(s):  
Major Element ◽  
Central Area ◽  
Igneous Rocks ◽  
Lava Flows ◽  
Primary Sources ◽  
Eastern Cape ◽  
Original Source ◽  
Geochemical Study ◽  
North Eastern ◽  
Area North

<p>Analyses in this dataset are from the following primary sources:</p> <p>Bowen, MP (1979) Some petrological aspects of the Omega Member flow unit, Barkly East District. Unpublished BSc Honours project, Rhodes University, 83pp.</p> <p>Pemberton, M (1979) A study of the massive unit of the Omega Member near Barkly East. Unpublished BSc Honours project, Rhodes University, 44pp</p> <p>Minne, HFD (1975) A study of a sequence of lava flows in the lower part of the Drakensberg Subgroup near Barkly East. Unpublished BSC Honours project, Rhodes University, 38pp</p> <p>Pemberton, J (1978) The geochemistry and petrology of Karoo basalts of the Barkly East area, north-eastern Cape. Unpublished MSc thesis, Rhodes University, 139pp</p> <p>Barrie, PD (1977) The Kraai River Formation: a petrographical and geochemical study of an occurrence in the vicinity of Barkly East. Unpublished BSC Honours project, Rhodes University.</p> <p>Major element analyses from original source. All trace elements redetermined in 2004.</p>

Ultramicroscopie petrographique; le rutile du quartz des granites

1964 ◽  
Vol S7-VI (2) ◽  
pp. 181-187 ◽  
Author(s):  
Georges Deicha
Keyword(s):  
Igneous Rocks ◽  
Geochemical Study ◽  
Important Means

Abstract Rutile needles of macroscopic, microscopic, and submicroscopic sizes occur in the quartz of acidic igneous rocks. Although it is not known whether they are present as the result of mechanical inclusion, crystallization simultaneous with that of the quartz, oriented exsolution, or replacement they are an important means of tectonic and geochemical study. A grain of granitic quartz torn by erosion from its crystalline petrographic context retains its submicroscopic inclusions throughout the course of its sedimentary peregrinations no matter how small the detrital fragments may become.

A geochemical study of Lewisian metasedimentary granulites and gneisses in the Scourie-Laxford area of the north-west Scotland

1983 ◽  
Vol 47 (342) ◽  
pp. 1-9 ◽  
Author(s):  
P. O. Okeke ◽  
G. D. Borley ◽  
J. Watson
Keyword(s):  
Trace Element ◽  
Igneous Rocks ◽  
Source Rocks ◽  
North West ◽  
Metasedimentary Rocks ◽  
The North ◽  
Granulite Metamorphism ◽  
Geochemical Study ◽  
High Pressure Granulite ◽  
Parent Rocks

AbstractMajor element, trace element, and REE data for metasedimentary granulites and their retrogressed derivatives formed from Archaean parent-rocks at two localities in the Lewisian complex of north-west Scotland are presented.The metasedimentary rocks are enclosed in and intruded by metatonalites and related calc-alkaline rocks and have been highly deformed and metamorphosed along with these rocks. They are geochemically distinct from this meta-igneous suite and range from highly aluminous to highly siliceous types. Comparisons of major and trace element data with those for unmetamorphosed Archaean and post-Archaean sediments suggest that they are derived from a detrital shale-greywacke assemblage, which may have included a volcaniclastic component. High ΣREE and ΣLREE suggest that the source-rocks included fractionated felsic igneous rocks.Evidence that depletion in the large ion lithophile elements K, Rb, Th accompanied high-pressure granulite metamorphism supports the view, based on data derived from the associated meta-igneous rocks, that depletion was effected by active fluids rather than by abstraction of a partial melt and suggests that removal of K and Th began only when a considerable reduction of Rb had taken place.

scholarly journals Les Roches Basiques Du Bas-Limousin (Massif Central Français) : Geochimie Et Implications Geodynamiques

2016 ◽  
Vol 12 (35) ◽  
pp. 382
Author(s):  
Jamil Ezzayani ◽  
Hassan El Hadi ◽  
Said Chakiri ◽  
Wafae Nouaim ◽  
Mohamed Allouza ◽  
...  
Keyword(s):  
Rare Earths ◽  
Regional Metamorphism ◽  
Igneous Rocks ◽  
Geochemical Data ◽  
Massif Central ◽  
Geochemical Study ◽  
Basic Rocks

The upper unit gneisses represent most of the Bas - Limousin. It is characterized by the intercalation of basic igneous rocks (metagabbro- and metadolerite). These are affected by regional metamorphism but primary textures are preserved. The aim of this work is to present new geochemical data, which allow characterizing the geochemical nature of these rocks and discussing their geodynamic meaning. Chemical analyzes of the major and traces elements were carried out at “Service commun des sciences de la terre de l’ Université de Nancy I”, rare earths elements were analyzed at CRPG of Nancy. The results of this geochemical study show that these basic rocks are comparable to continental tholeiitic rocks.

Sign in / Sign up

Export Citation Format

Share Document