Open main menu
Home
Random
Recent changes
Special pages
Community portal
Preferences
About Wikipedia
Disclaimers
Incubator escapee wiki
Search
User menu
Talk
Dark mode
Contributions
Create account
Log in
Editing
Granitoid
(section)
Warning:
You are not logged in. Your IP address will be publicly visible if you make any edits. If you
log in
or
create an account
, your edits will be attributed to your username, along with other benefits.
Anti-spam check. Do
not
fill this in!
{{Short description|Category of coarse-grained igneous rocks}} [[File:Granite.jpg|thumb|Granite rock hand-sized sample]] A '''granitoid''' is a broad term referring to a diverse group of coarse-grained igneous rocks that are widely distributed across the globe, covering a significant portion of the Earth's exposed surface and constituting a large part of the continental crust.<ref>{{Cite journal |last=Tomás |first=R. |last2=Cano |first2=M. |last3=Pulgarín |first3=L. F. |last4=Brotóns |first4=V. |last5=Benavente |first5=D. |last6=Miranda |first6=T. |last7=Vasconcelos |first7=G. |date=2021-11-01 |title=Thermal effect of high temperatures on the physical and mechanical properties of a granite used in UNESCO World Heritage sites in north Portugal |url=https://linkinghub.elsevier.com/retrieve/pii/S2352710221006811 |journal=Journal of Building Engineering |volume=43 |pages=102823 |doi=10.1016/j.jobe.2021.102823 |issn=2352-7102|hdl=10045/115630 |hdl-access=free }}</ref> These rocks are primarily composed of [[quartz]], [[plagioclase]], and [[alkali feldspar]].<ref>{{cite web | url=https://mrdata.usgs.gov/catalog/science.php?thcode=4&term=4.4 | title=USGS: Mineral Resources On-Line Spatial Data: Granitoid }}</ref> Granitoids range from plagioclase-rich [[tonalite]]s to alkali-rich [[syenite]]s and from quartz-poor [[monzonite]]s to quartz-rich [[quartzolite]]s.<ref name="Streckeisen-1974">{{cite journal |last=Streckeisen |first=A. |year=1974 |title=Classification and Nomenclature of Plutonic Rocks: Recommendations of the IUGS Subcommission on the Systematics of Igneous Rocks |journal=Geologische Rundschau |volume=63 |issue=2 |pages=773–86 |bibcode=1974GeoRu..63..773S |doi=10.1007/BF01820841 |s2cid=130569261 |language=de}}</ref> As only two of the three defining mineral groups (quartz, plagioclase, and alkali feldspar) need to be present for the rock to be called a granitoid, [[feldspathoid|foid]]-bearing rocks, which predominantly contain feldspars but no quartz, are also granitoids.<ref name="Streckeisen-1974" />
Edit summary
(Briefly describe your changes)
By publishing changes, you agree to the
Terms of Use
, and you irrevocably agree to release your contribution under the
CC BY-SA 4.0 License
and the
GFDL
. You agree that a hyperlink or URL is sufficient attribution under the Creative Commons license.
Cancel
Editing help
(opens in new window)