Latest Eocene and Oligocene tectonic controls on carbonate deposition in eastern Java and the south Makassar Straits, Indonesia

This review examines the development of carbonates and their enclosing siliciclastic sediments, from the Late Eocene until the end of the Oligocene, in eastern Java and the southern Makassar Straits. Five genetic sedimentary sequences are recognised, which correlate to other studies in the area, and...
Ausführliche Beschreibung

Gespeichert in:

Autor*in:	Luan, Xiwu [verfasserIn] Lunt, Peter [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2021

Schlagwörter:	SE Asia Basin analysis Oligocene Oligo-Miocene boundary Tectono-stratigraphy Geohistory

Übergeordnetes Werk:	Enthalten in: Journal of Asian earth sciences - Amsterdam [u.a.] : Elsevier Science, 1997, 220
Übergeordnetes Werk:	volume:220

DOI / URN:	10.1016/j.jseaes.2021.104900

Katalog-ID:	ELV006692702

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allfields	10.1016/j.jseaes.2021.104900 doi (DE-627)ELV006692702 (ELSEVIER)S1367-9120(21)00238-8 DE-627 ger DE-627 rda eng 550 DE-600 38.00 bkl Luan, Xiwu verfasserin (orcid)0000-0003-4874-241X aut Latest Eocene and Oligocene tectonic controls on carbonate deposition in eastern Java and the south Makassar Straits, Indonesia 2021 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier This review examines the development of carbonates and their enclosing siliciclastic sediments, from the Late Eocene until the end of the Oligocene, in eastern Java and the southern Makassar Straits. Five genetic sedimentary sequences are recognised, which correlate to other studies in the area, and points to an episodic sedimentary history controlled by tectonism. An additional intra Late Miocene uplift and unconformity is also described as it illustrates the speed at which tectonic transitions occurred. These genetic sedimentary sequences are part of a regional stratigraphic framework that describes the tectonic evolution of Sundaland. Two unconformities, in mid-Oligocene and at terminal Oligocene times, correlating across the entire eastern margin of Sundaland, are highlighted as part of a new regional tectonic model. SE Asia Basin analysis Oligocene Oligo-Miocene boundary Tectono-stratigraphy Geohistory Lunt, Peter verfasserin aut Enthalten in Journal of Asian earth sciences Amsterdam [u.a.] : Elsevier Science, 1997 220 Online-Ressource (DE-627)303391960 (DE-600)1494743-2 (DE-576)106846035 1878-5786 nnns volume:220 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.00 Geowissenschaften: Allgemeines AR 220
spelling	10.1016/j.jseaes.2021.104900 doi (DE-627)ELV006692702 (ELSEVIER)S1367-9120(21)00238-8 DE-627 ger DE-627 rda eng 550 DE-600 38.00 bkl Luan, Xiwu verfasserin (orcid)0000-0003-4874-241X aut Latest Eocene and Oligocene tectonic controls on carbonate deposition in eastern Java and the south Makassar Straits, Indonesia 2021 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier This review examines the development of carbonates and their enclosing siliciclastic sediments, from the Late Eocene until the end of the Oligocene, in eastern Java and the southern Makassar Straits. Five genetic sedimentary sequences are recognised, which correlate to other studies in the area, and points to an episodic sedimentary history controlled by tectonism. An additional intra Late Miocene uplift and unconformity is also described as it illustrates the speed at which tectonic transitions occurred. These genetic sedimentary sequences are part of a regional stratigraphic framework that describes the tectonic evolution of Sundaland. Two unconformities, in mid-Oligocene and at terminal Oligocene times, correlating across the entire eastern margin of Sundaland, are highlighted as part of a new regional tectonic model. SE Asia Basin analysis Oligocene Oligo-Miocene boundary Tectono-stratigraphy Geohistory Lunt, Peter verfasserin aut Enthalten in Journal of Asian earth sciences Amsterdam [u.a.] : Elsevier Science, 1997 220 Online-Ressource (DE-627)303391960 (DE-600)1494743-2 (DE-576)106846035 1878-5786 nnns volume:220 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.00 Geowissenschaften: Allgemeines AR 220
allfields_unstemmed	10.1016/j.jseaes.2021.104900 doi (DE-627)ELV006692702 (ELSEVIER)S1367-9120(21)00238-8 DE-627 ger DE-627 rda eng 550 DE-600 38.00 bkl Luan, Xiwu verfasserin (orcid)0000-0003-4874-241X aut Latest Eocene and Oligocene tectonic controls on carbonate deposition in eastern Java and the south Makassar Straits, Indonesia 2021 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier This review examines the development of carbonates and their enclosing siliciclastic sediments, from the Late Eocene until the end of the Oligocene, in eastern Java and the southern Makassar Straits. Five genetic sedimentary sequences are recognised, which correlate to other studies in the area, and points to an episodic sedimentary history controlled by tectonism. An additional intra Late Miocene uplift and unconformity is also described as it illustrates the speed at which tectonic transitions occurred. These genetic sedimentary sequences are part of a regional stratigraphic framework that describes the tectonic evolution of Sundaland. Two unconformities, in mid-Oligocene and at terminal Oligocene times, correlating across the entire eastern margin of Sundaland, are highlighted as part of a new regional tectonic model. SE Asia Basin analysis Oligocene Oligo-Miocene boundary Tectono-stratigraphy Geohistory Lunt, Peter verfasserin aut Enthalten in Journal of Asian earth sciences Amsterdam [u.a.] : Elsevier Science, 1997 220 Online-Ressource (DE-627)303391960 (DE-600)1494743-2 (DE-576)106846035 1878-5786 nnns volume:220 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.00 Geowissenschaften: Allgemeines AR 220
allfieldsGer	10.1016/j.jseaes.2021.104900 doi (DE-627)ELV006692702 (ELSEVIER)S1367-9120(21)00238-8 DE-627 ger DE-627 rda eng 550 DE-600 38.00 bkl Luan, Xiwu verfasserin (orcid)0000-0003-4874-241X aut Latest Eocene and Oligocene tectonic controls on carbonate deposition in eastern Java and the south Makassar Straits, Indonesia 2021 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier This review examines the development of carbonates and their enclosing siliciclastic sediments, from the Late Eocene until the end of the Oligocene, in eastern Java and the southern Makassar Straits. Five genetic sedimentary sequences are recognised, which correlate to other studies in the area, and points to an episodic sedimentary history controlled by tectonism. An additional intra Late Miocene uplift and unconformity is also described as it illustrates the speed at which tectonic transitions occurred. These genetic sedimentary sequences are part of a regional stratigraphic framework that describes the tectonic evolution of Sundaland. Two unconformities, in mid-Oligocene and at terminal Oligocene times, correlating across the entire eastern margin of Sundaland, are highlighted as part of a new regional tectonic model. SE Asia Basin analysis Oligocene Oligo-Miocene boundary Tectono-stratigraphy Geohistory Lunt, Peter verfasserin aut Enthalten in Journal of Asian earth sciences Amsterdam [u.a.] : Elsevier Science, 1997 220 Online-Ressource (DE-627)303391960 (DE-600)1494743-2 (DE-576)106846035 1878-5786 nnns volume:220 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.00 Geowissenschaften: Allgemeines AR 220
allfieldsSound	10.1016/j.jseaes.2021.104900 doi (DE-627)ELV006692702 (ELSEVIER)S1367-9120(21)00238-8 DE-627 ger DE-627 rda eng 550 DE-600 38.00 bkl Luan, Xiwu verfasserin (orcid)0000-0003-4874-241X aut Latest Eocene and Oligocene tectonic controls on carbonate deposition in eastern Java and the south Makassar Straits, Indonesia 2021 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier This review examines the development of carbonates and their enclosing siliciclastic sediments, from the Late Eocene until the end of the Oligocene, in eastern Java and the southern Makassar Straits. Five genetic sedimentary sequences are recognised, which correlate to other studies in the area, and points to an episodic sedimentary history controlled by tectonism. An additional intra Late Miocene uplift and unconformity is also described as it illustrates the speed at which tectonic transitions occurred. These genetic sedimentary sequences are part of a regional stratigraphic framework that describes the tectonic evolution of Sundaland. Two unconformities, in mid-Oligocene and at terminal Oligocene times, correlating across the entire eastern margin of Sundaland, are highlighted as part of a new regional tectonic model. SE Asia Basin analysis Oligocene Oligo-Miocene boundary Tectono-stratigraphy Geohistory Lunt, Peter verfasserin aut Enthalten in Journal of Asian earth sciences Amsterdam [u.a.] : Elsevier Science, 1997 220 Online-Ressource (DE-627)303391960 (DE-600)1494743-2 (DE-576)106846035 1878-5786 nnns volume:220 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.00 Geowissenschaften: Allgemeines AR 220
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author	Luan, Xiwu
spellingShingle	Luan, Xiwu ddc 550 bkl 38.00 misc SE Asia misc Basin analysis misc Oligocene misc Oligo-Miocene boundary misc Tectono-stratigraphy misc Geohistory Latest Eocene and Oligocene tectonic controls on carbonate deposition in eastern Java and the south Makassar Straits, Indonesia
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topic_title	550 DE-600 38.00 bkl Latest Eocene and Oligocene tectonic controls on carbonate deposition in eastern Java and the south Makassar Straits, Indonesia SE Asia Basin analysis Oligocene Oligo-Miocene boundary Tectono-stratigraphy Geohistory
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title	Latest Eocene and Oligocene tectonic controls on carbonate deposition in eastern Java and the south Makassar Straits, Indonesia
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title_full	Latest Eocene and Oligocene tectonic controls on carbonate deposition in eastern Java and the south Makassar Straits, Indonesia
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title_sort	latest eocene and oligocene tectonic controls on carbonate deposition in eastern java and the south makassar straits, indonesia
title_auth	Latest Eocene and Oligocene tectonic controls on carbonate deposition in eastern Java and the south Makassar Straits, Indonesia
abstract	This review examines the development of carbonates and their enclosing siliciclastic sediments, from the Late Eocene until the end of the Oligocene, in eastern Java and the southern Makassar Straits. Five genetic sedimentary sequences are recognised, which correlate to other studies in the area, and points to an episodic sedimentary history controlled by tectonism. An additional intra Late Miocene uplift and unconformity is also described as it illustrates the speed at which tectonic transitions occurred. These genetic sedimentary sequences are part of a regional stratigraphic framework that describes the tectonic evolution of Sundaland. Two unconformities, in mid-Oligocene and at terminal Oligocene times, correlating across the entire eastern margin of Sundaland, are highlighted as part of a new regional tectonic model.
abstractGer	This review examines the development of carbonates and their enclosing siliciclastic sediments, from the Late Eocene until the end of the Oligocene, in eastern Java and the southern Makassar Straits. Five genetic sedimentary sequences are recognised, which correlate to other studies in the area, and points to an episodic sedimentary history controlled by tectonism. An additional intra Late Miocene uplift and unconformity is also described as it illustrates the speed at which tectonic transitions occurred. These genetic sedimentary sequences are part of a regional stratigraphic framework that describes the tectonic evolution of Sundaland. Two unconformities, in mid-Oligocene and at terminal Oligocene times, correlating across the entire eastern margin of Sundaland, are highlighted as part of a new regional tectonic model.
abstract_unstemmed	This review examines the development of carbonates and their enclosing siliciclastic sediments, from the Late Eocene until the end of the Oligocene, in eastern Java and the southern Makassar Straits. Five genetic sedimentary sequences are recognised, which correlate to other studies in the area, and points to an episodic sedimentary history controlled by tectonism. An additional intra Late Miocene uplift and unconformity is also described as it illustrates the speed at which tectonic transitions occurred. These genetic sedimentary sequences are part of a regional stratigraphic framework that describes the tectonic evolution of Sundaland. Two unconformities, in mid-Oligocene and at terminal Oligocene times, correlating across the entire eastern margin of Sundaland, are highlighted as part of a new regional tectonic model.
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title_short	Latest Eocene and Oligocene tectonic controls on carbonate deposition in eastern Java and the south Makassar Straits, Indonesia
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doi_str	10.1016/j.jseaes.2021.104900
up_date	2024-07-06T22:14:38.274Z
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