Jamaludin, Siti Nur Fathiyah and Ibrahim, Noor Azahar (2025) PEGMATITE. [Instructional Teaching Materials]
![[thumbnail of 335x386.png]](http://utpedia.utp.edu.my/style/images/fileicons/image.png)
335x386.png
Restricted to Registered users only
Download (1MB)
![[thumbnail of The upstream rare earth resources of Malaysia- Insight into geology,.pdf]](http://utpedia.utp.edu.my/style/images/fileicons/text.png)
The upstream rare earth resources of Malaysia- Insight into geology,.pdf
Restricted to Registered users only
Download (7MB)
Abstract
Major Rock Type: Igneous
Formation: Jerai Formation
Age: Cambrian (540 - 485 million years ago)
Origin: Singkir Darat, Yan, Kedah
* This rock has been extracted from the Singkir Darat Quarry in Yan, Kedah, known as pegmatite, is a fascinating geological specimen with a unique composition and structure. It was dated that the age of this rock was from Cambrian Period, approximately 540 to 485 million years ago.
* Pegmatite is an igneous rock which has a mineral composition similar to granite. The predominant mineral constituents are quartz and feldspar, creating a beautiful interlocking of colours and textures.
* The quartz crystals, often translucent and colossal while the feldspar crystals exhibit a creamy white hue. These minerals are accompanied by the presence of mica minerals like muscovite and biotite, contributing their shiny, flaky appearance to the rock.
* The only difference is that pegmatite has larger sized minerals and these minerals can be easily observed in the pegmatite boulders.
* Pegmatite minerals grow to unusually large sizes due to the exceptionally slow cooling process during their formation, allowing crystals to reach several meters in length.
Item Type: | Instructional Teaching Materials |
---|---|
Depositing User: | Mr Ahmad Suhairi Mohamed Lazim |
Date Deposited: | 14 Feb 2025 08:12 |
Last Modified: | 30 Jun 2025 10:26 |
URI: | http://utpedia.utp.edu.my/id/eprint/30242 |