Cover Image

GENERAL GEOLOGY OF SEMANGGOL AREA TRANSECT ALONG JALAN KAMUNTING AT SUNGAI AIR HITAM PALEO-DEPOSITIONAL INTERPRETATION OF THE LITHOLOGS/FIELD OBSERVATION WITH EMPHASIS ON DOMINANT STRUCTURAL BEHAVIOUR

Malay Peninsula is linked towards two continental terrane, Sibumasu (western belt of the peninsula) and Sukhothai arc (Central and Eastern belt of the peninsula). Due to collision, Malay Peninsula was formed and accretionary prism form Bentong-Raub suture zone. Metcalfe stated that based on data col...

Full description

Saved in:
Bibliographic Details
Main Author: BIN NASRUDIN , NADZRIL IZZUDIN
Format: Final Year Project
Language:English
Published: Universiti Teknologi PETRONAS 2014
Subjects:
G Geography (General)
Online Access:http://utpedia.utp.edu.my/18279/1/Nadzril%20Izzudin%20Nasrudin_15545_FYP2_Sept_2014_Dissertation.pdf
http://utpedia.utp.edu.my/18279/
Tags: Add Tag
No Tags, Be the first to tag this record!
id my-utp-utpedia.18279
record_format eprints
spelling my-utp-utpedia.182792018-11-22T14:41:51Z http://utpedia.utp.edu.my/18279/ GENERAL GEOLOGY OF SEMANGGOL AREA TRANSECT ALONG JALAN KAMUNTING AT SUNGAI AIR HITAM PALEO-DEPOSITIONAL INTERPRETATION OF THE LITHOLOGS/FIELD OBSERVATION WITH EMPHASIS ON DOMINANT STRUCTURAL BEHAVIOUR BIN NASRUDIN , NADZRIL IZZUDIN G Geography (General) Malay Peninsula is linked towards two continental terrane, Sibumasu (western belt of the peninsula) and Sukhothai arc (Central and Eastern belt of the peninsula). Due to collision, Malay Peninsula was formed and accretionary prism form Bentong-Raub suture zone. Metcalfe stated that based on data collected has deduced that the origin of sibumasu is part of the NW Australian gondwana border during Cambrian-early Permian. The age of Semanggol formation is deduced as late Early Permian to late Triassic as (chert sequence of Early Triassic was not completed). Depending on the radiolarians, the age is said as late Early Permian to Middle Triassic. Three units of facies available in Semanggol formation: Chert, conglomerate and Rhythmic facies. Semanggol formation consists of three separate sections; Northern, Central and Southern. Most research has been conducted in Northern and Central in Kedah. Southern part of Semanggol is the least studied. Last carried out by Burton (1970) towards this recent mapping project. The analysis and construction of a geological map and propose tectonic model will contribute to enhancing and update geological information of the location. Universiti Teknologi PETRONAS 2014-09 Final Year Project NonPeerReviewed application/pdf en http://utpedia.utp.edu.my/18279/1/Nadzril%20Izzudin%20Nasrudin_15545_FYP2_Sept_2014_Dissertation.pdf BIN NASRUDIN , NADZRIL IZZUDIN (2014) GENERAL GEOLOGY OF SEMANGGOL AREA TRANSECT ALONG JALAN KAMUNTING AT SUNGAI AIR HITAM PALEO-DEPOSITIONAL INTERPRETATION OF THE LITHOLOGS/FIELD OBSERVATION WITH EMPHASIS ON DOMINANT STRUCTURAL BEHAVIOUR. Universiti Teknologi PETRONAS. (Submitted)
institution Universiti Teknologi Petronas
building UTP Resource Centre
collection Institutional Repository
continent Asia
country Malaysia
content_provider Universiti Teknologi Petronas
content_source UTP Electronic and Digitized Intellectual Asset
url_provider http://utpedia.utp.edu.my/
language English
topic G Geography (General)
spellingShingle G Geography (General)
BIN NASRUDIN , NADZRIL IZZUDIN
GENERAL GEOLOGY OF SEMANGGOL AREA TRANSECT ALONG JALAN KAMUNTING AT SUNGAI AIR HITAM PALEO-DEPOSITIONAL INTERPRETATION OF THE LITHOLOGS/FIELD OBSERVATION WITH EMPHASIS ON DOMINANT STRUCTURAL BEHAVIOUR
description Malay Peninsula is linked towards two continental terrane, Sibumasu (western belt of the peninsula) and Sukhothai arc (Central and Eastern belt of the peninsula). Due to collision, Malay Peninsula was formed and accretionary prism form Bentong-Raub suture zone. Metcalfe stated that based on data collected has deduced that the origin of sibumasu is part of the NW Australian gondwana border during Cambrian-early Permian. The age of Semanggol formation is deduced as late Early Permian to late Triassic as (chert sequence of Early Triassic was not completed). Depending on the radiolarians, the age is said as late Early Permian to Middle Triassic. Three units of facies available in Semanggol formation: Chert, conglomerate and Rhythmic facies. Semanggol formation consists of three separate sections; Northern, Central and Southern. Most research has been conducted in Northern and Central in Kedah. Southern part of Semanggol is the least studied. Last carried out by Burton (1970) towards this recent mapping project. The analysis and construction of a geological map and propose tectonic model will contribute to enhancing and update geological information of the location.
format Final Year Project
author BIN NASRUDIN , NADZRIL IZZUDIN
author_facet BIN NASRUDIN , NADZRIL IZZUDIN
author_sort BIN NASRUDIN , NADZRIL IZZUDIN
title GENERAL GEOLOGY OF SEMANGGOL AREA TRANSECT ALONG JALAN KAMUNTING AT SUNGAI AIR HITAM PALEO-DEPOSITIONAL INTERPRETATION OF THE LITHOLOGS/FIELD OBSERVATION WITH EMPHASIS ON DOMINANT STRUCTURAL BEHAVIOUR
title_short GENERAL GEOLOGY OF SEMANGGOL AREA TRANSECT ALONG JALAN KAMUNTING AT SUNGAI AIR HITAM PALEO-DEPOSITIONAL INTERPRETATION OF THE LITHOLOGS/FIELD OBSERVATION WITH EMPHASIS ON DOMINANT STRUCTURAL BEHAVIOUR
title_full GENERAL GEOLOGY OF SEMANGGOL AREA TRANSECT ALONG JALAN KAMUNTING AT SUNGAI AIR HITAM PALEO-DEPOSITIONAL INTERPRETATION OF THE LITHOLOGS/FIELD OBSERVATION WITH EMPHASIS ON DOMINANT STRUCTURAL BEHAVIOUR
title_fullStr GENERAL GEOLOGY OF SEMANGGOL AREA TRANSECT ALONG JALAN KAMUNTING AT SUNGAI AIR HITAM PALEO-DEPOSITIONAL INTERPRETATION OF THE LITHOLOGS/FIELD OBSERVATION WITH EMPHASIS ON DOMINANT STRUCTURAL BEHAVIOUR
title_full_unstemmed GENERAL GEOLOGY OF SEMANGGOL AREA TRANSECT ALONG JALAN KAMUNTING AT SUNGAI AIR HITAM PALEO-DEPOSITIONAL INTERPRETATION OF THE LITHOLOGS/FIELD OBSERVATION WITH EMPHASIS ON DOMINANT STRUCTURAL BEHAVIOUR
title_sort general geology of semanggol area transect along jalan kamunting at sungai air hitam paleo-depositional interpretation of the lithologs/field observation with emphasis on dominant structural behaviour
publisher Universiti Teknologi PETRONAS
publishDate 2014
url http://utpedia.utp.edu.my/18279/1/Nadzril%20Izzudin%20Nasrudin_15545_FYP2_Sept_2014_Dissertation.pdf
http://utpedia.utp.edu.my/18279/
_version_ 1739832484836671488
score 13.211869

Similar Items