Aptian to turonian radiolarians from chert blocks in the Kuamut Melange, Sabah, Malaysia

The Kuamut Melange is located in the Kunak district, southeast Sabah. The mélange consists of clasts and blocks of broken Paleogene formations, and dismembered ophiolite blocks embedded in shale matrix. Fourteen samples were collected from sections S1 and S2 of the Kuamut Melange. A total of 45 spec...

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Main Authors: Basir Jasin, Junaidi Asis
Format: Article
Language:English
Published: Universiti Kebangsaan Malaysia 2013
Online Access:http://journalarticle.ukm.my/6148/
http://journalarticle.ukm.my/6148/
http://journalarticle.ukm.my/6148/1/02_Junaidi-1.pdf
id ukm-6148
recordtype eprints
spelling ukm-61482016-12-14T06:40:28Z http://journalarticle.ukm.my/6148/ Aptian to turonian radiolarians from chert blocks in the Kuamut Melange, Sabah, Malaysia Basir Jasin, Junaidi Asis, The Kuamut Melange is located in the Kunak district, southeast Sabah. The mélange consists of clasts and blocks of broken Paleogene formations, and dismembered ophiolite blocks embedded in shale matrix. Fourteen samples were collected from sections S1 and S2 of the Kuamut Melange. A total of 45 species of radiolarians have been identified and only 36 selected species are used for age determination. Three assemblages (I-III) were identified. Assemblage I consists of Dictyomitra excellence, Crucella bossoensis, Hiscocapsa asseni, Hexapyramis precedis, Thanarla brouweri, Acanthocircus levis, Obeliscoites vinassai, Stichomitra communis, Staurosphaeretta longispina, Xitus spicularius, Triactoma cellulosa, and Dactyliosphaera maxima. This assemblage is marked by the occurrence of Crucella gavalai indicative of Aptian to Albian in age. Assemblage II was characterized by zonal maker Xitus mclaughlini. Other species in this assemblage are Xitus spinosus, Stichomitra tosaensis, Dictyomitra gracilis, Dictyomitra montisserei, Pseudodictyomitra pseudomacrocephala, Pessagnobrachia fabianii, Crucella messinae, Tuguriella pagoda, Dictyomitra obesa, Triactoma paronai, Rhopalosyringium euganeum, Acanthocircus venetus, Acaeniotyle rebelis, Dictyomitra formosa, Pseudodictyomitra tiara and Patellula helios. This assemblage ranges from Albian to Cenomanian. Assemblages III is represented by zonal maker Crucella cachensis and others species in this assemblage are Hemicryptocapsa polyhedra, Eostichomitra bonum, Pseudotheocampe tina, Ultranapora cretacea and Alievium superbum. Assemblage III is Turonian in age. The radiolarian assemblages suggest that the age of chert blocks ranges from Aptian to Turonian, Cretaceous. The cherts were originally deposited on an oceanic crust of a marginal basin during Cretaceous and were tectonically deformed to form melange in Miocene time. Universiti Kebangsaan Malaysia 2013-05 Article PeerReviewed application/pdf en http://journalarticle.ukm.my/6148/1/02_Junaidi-1.pdf Basir Jasin, and Junaidi Asis, (2013) Aptian to turonian radiolarians from chert blocks in the Kuamut Melange, Sabah, Malaysia. Sains Malaysiana, 42 (5). pp. 561-570. ISSN 0126-6039 http://www.ukm.my/jsm/
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description The Kuamut Melange is located in the Kunak district, southeast Sabah. The mélange consists of clasts and blocks of broken Paleogene formations, and dismembered ophiolite blocks embedded in shale matrix. Fourteen samples were collected from sections S1 and S2 of the Kuamut Melange. A total of 45 species of radiolarians have been identified and only 36 selected species are used for age determination. Three assemblages (I-III) were identified. Assemblage I consists of Dictyomitra excellence, Crucella bossoensis, Hiscocapsa asseni, Hexapyramis precedis, Thanarla brouweri, Acanthocircus levis, Obeliscoites vinassai, Stichomitra communis, Staurosphaeretta longispina, Xitus spicularius, Triactoma cellulosa, and Dactyliosphaera maxima. This assemblage is marked by the occurrence of Crucella gavalai indicative of Aptian to Albian in age. Assemblage II was characterized by zonal maker Xitus mclaughlini. Other species in this assemblage are Xitus spinosus, Stichomitra tosaensis, Dictyomitra gracilis, Dictyomitra montisserei, Pseudodictyomitra pseudomacrocephala, Pessagnobrachia fabianii, Crucella messinae, Tuguriella pagoda, Dictyomitra obesa, Triactoma paronai, Rhopalosyringium euganeum, Acanthocircus venetus, Acaeniotyle rebelis, Dictyomitra formosa, Pseudodictyomitra tiara and Patellula helios. This assemblage ranges from Albian to Cenomanian. Assemblages III is represented by zonal maker Crucella cachensis and others species in this assemblage are Hemicryptocapsa polyhedra, Eostichomitra bonum, Pseudotheocampe tina, Ultranapora cretacea and Alievium superbum. Assemblage III is Turonian in age. The radiolarian assemblages suggest that the age of chert blocks ranges from Aptian to Turonian, Cretaceous. The cherts were originally deposited on an oceanic crust of a marginal basin during Cretaceous and were tectonically deformed to form melange in Miocene time.
format Article
author Basir Jasin,
Junaidi Asis,
spellingShingle Basir Jasin,
Junaidi Asis,
Aptian to turonian radiolarians from chert blocks in the Kuamut Melange, Sabah, Malaysia
author_facet Basir Jasin,
Junaidi Asis,
author_sort Basir Jasin,
title Aptian to turonian radiolarians from chert blocks in the Kuamut Melange, Sabah, Malaysia
title_short Aptian to turonian radiolarians from chert blocks in the Kuamut Melange, Sabah, Malaysia
title_full Aptian to turonian radiolarians from chert blocks in the Kuamut Melange, Sabah, Malaysia
title_fullStr Aptian to turonian radiolarians from chert blocks in the Kuamut Melange, Sabah, Malaysia
title_full_unstemmed Aptian to turonian radiolarians from chert blocks in the Kuamut Melange, Sabah, Malaysia
title_sort aptian to turonian radiolarians from chert blocks in the kuamut melange, sabah, malaysia
publisher Universiti Kebangsaan Malaysia
publishDate 2013
url http://journalarticle.ukm.my/6148/
http://journalarticle.ukm.my/6148/
http://journalarticle.ukm.my/6148/1/02_Junaidi-1.pdf
first_indexed 2023-09-18T19:46:07Z
last_indexed 2023-09-18T19:46:07Z
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