General geology of Renyok Waterfall with emphasize on the mineralogy and petrology of leucogranite and metasediments (enclaves) Musli Ani Cohlli.

By: Musli Ani CohlliMaterial type: TextTextPublisher: 2011Description: xii, 103p. col., ill., maps 30cmSubject(s): Mineralogy -- Kelantan -- Air Terjun Renyok | Petrology -- Kelantan -- Air Terjun Renyok | Geology -- Kelantan -- Air Terjun Renyok | Air Terjun Renyok (Jeli, Kelantan)Summary: The study area located at Renyok Waterfall, Jeli, Kelantan exposed near TNB mini power station. This area is part of late Cretaceous Kenerong Leucogranite, a component of Stong Complex consists of leucogranite vein and high grade metasedimentary enclaves. The main objective of this project is to study the petrology any mineralogy of both granite and metamorphic rocks.
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April 2011.

Includes bibliographical references

The study area located at Renyok Waterfall, Jeli, Kelantan exposed near TNB mini power station. This area is part of late Cretaceous Kenerong Leucogranite, a component of Stong Complex consists of leucogranite vein and high grade metasedimentary enclaves. The main objective of this project is to study the petrology any mineralogy of both granite and metamorphic rocks.

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