Abstracts - faqs.org

Abstracts

Earth sciences

Search abstracts:
Abstracts » Earth sciences

The nodular granite of Castanheira, north central Portugal: origin of the nodules and evidence for diapiric mobilization of granite

Article Abstract:

The Hercynian Castaniera pluton of north-central Portugal is a small granitic intrusion containing an abundance of nodular granites rimmed with biotites. The nodules are believed to represent the original cavities in the topmost volatile-rich areas of the pluton. The biotite rims areinferred to be of magmatic origin as shown by the depletion of K and Rb in the host granite. Analysis of the shapes of the nodules have lead to a conclusion that the Castanheira pluton was a diapirically emplaced low viscocity facies of the larger granitic Serra de Freita pluton.

Author: Reavy,R.J., Hutton, D.W.H., Finch, A.A.
Publisher: Cambridge University Press
Publication Name: Geological Magazine
Subject: Earth sciences
ISSN: 0016-7568
Year: 1993
Portugal, Granite, Diapirs

User Contributions:

Comment about this article or add new information about this topic:

CAPTCHA


Emplacement and thermal metamorphism associated with the post-orogenic strath ossian pluton, grampian highlands, Scotland

Article Abstract:

The metasedimentary rocks of the Neoproterozoic Grampian and Appin groups were encroached upon by the multiphase Strath Ossian Pluton during the Silurian or early Devonian times. The emplacement that took place during the post-organic regional uplift and cooling followed the main ductile tectono-thermal history. Magmatization of the rocks in the northern part of the pluton with the generation of new ductile structures occurred due to the early emplacement of the diorite magma.

Author: Key, R.M., Phillips, E.R., Chacksfield, B.C.
Publisher: Cambridge University Press
Publication Name: Geological Magazine
Subject: Earth sciences
ISSN: 0016-7568
Year: 1993
Scotland

User Contributions:

Comment about this article or add new information about this topic:

CAPTCHA


The Lower Cambrian Wrekin Quartzite and the age of its unconformity on the Ercall Granophyre

Article Abstract:

Acritarch specimens were found on the clay horizon above the unconformity between the Lower Cambrian Wrekin Quartzite and the Ercall Granophyre. The specimens were dated and used in relation to age determination of the granophyre intrusion and the unconformity. Stratigraphic findings and age determination have shown that the intrusion occurred 560 plus or minus one Ma. However the Cambrian Unconformity is younger than 533 plus or minus 13 Ma.

Author: Wright, A.E., Fairchild, I.J., Moseley, F., Downie, C.
Publisher: Cambridge University Press
Publication Name: Geological Magazine
Subject: Earth sciences
ISSN: 0016-7568
Year: 1993
Analysis, Stratigraphic correlation, Geology, Stratigraphic, Correlation (Geology), Stratigraphy, Cambrian period, Quartzite

User Contributions:

Comment about this article or add new information about this topic:

CAPTCHA


Subjects list: Research, Natural history, Intrusions (Geology)
Similar abstracts:
  • Abstracts: Quaternary convergent margin tectonics of Costa Rica, segmentation of the Cocos Plate, and Central American volcanism
  • Abstracts: The role of neighborhood competition in the spacing and diversity of ant communities. Regulation of "momentary" diversity by dominant species in exceptionally rich ant communities of the Australian seasonal tropics
  • Abstracts: Loss of isotopic (Nd,O) and chemical (REE) memory during metamorphism of komatiites: new evidence from eastern Finland
  • Abstracts: Veins in the Locksport dolostone: evidence for an Acadian fluid circulation system. Termination of a continental-scale strike-slip fault in partially melted crust: the West Pernambuco shear zone, northeast Brazil
  • Abstracts: Implications of a Bengal Fan-type deposit in the Paleozoic Lachlan fold belt of southeastern Australia. Slow late Paleozoic exhumation in the Presidential Range of New Hampshire as determined by the 40Ar/39Ar relief method: comment and reply
This website is not affiliated with document authors or copyright owners. This page is provided for informational purposes only. Unintentional errors are possible.
Some parts © 2025 Advameg, Inc.