Detrital zircon geochronology and related evidence from clastic sediments in the Kyrenia Range, N Cyprus: Implications for the Mesozoic-Cenozoic erosional history and tectonics of southern Anatolia

Triassic to Pleistocene sandstones of the Kyrenia Range, N Cyprus provide an exceptional repository of the erosional history of Anatolia. The Kyrenia Range features several different tectonic hypotheses concerning the Eastern Mediterranean region, which are tested here using a combination of new and...
Ausführliche Beschreibung

Gespeichert in:

Autor*in:	Chen, Guohui [verfasserIn] Robertson, Alastair H.F. [verfasserIn] Wu, Fu-Yuan [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2022

Schlagwörter:	Eastern Mediterranean Kyrenia Range U-Pb zircon dating Hf isotopic analysis Sediment provenance Tectonic synthesis

Übergeordnetes Werk:	Enthalten in: Earth science reviews - Amsterdam [u.a.] : Elsevier, 1966, 233
Übergeordnetes Werk:	volume:233

DOI / URN:	10.1016/j.earscirev.2022.104167

Katalog-ID:	ELV008571864

Internformat


LEADER	01000caa a22002652 4500
001	ELV008571864
003	DE-627
005	20230530142410.0
007	cr uuu---uuuuu
008	230509s2022 xx \|\|\|\|\|o 00\| \|\|eng c
024	7		\|a 10.1016/j.earscirev.2022.104167 \|2 doi
035			\|a (DE-627)ELV008571864
035			\|a (ELSEVIER)S0012-8252(22)00251-3
040			\|a DE-627 \|b ger \|c DE-627 \|e rda
041			\|a eng
082	0	4	\|a 550 \|q VZ
084			\|a 38.00 \|2 bkl
100	1		\|a Chen, Guohui \|e verfasserin \|4 aut
245	1	0	\|a Detrital zircon geochronology and related evidence from clastic sediments in the Kyrenia Range, N Cyprus: Implications for the Mesozoic-Cenozoic erosional history and tectonics of southern Anatolia
264		1	\|c 2022
336			\|a nicht spezifiziert \|b zzz \|2 rdacontent
337			\|a Computermedien \|b c \|2 rdamedia
338			\|a Online-Ressource \|b cr \|2 rdacarrier
520			\|a Triassic to Pleistocene sandstones of the Kyrenia Range, N Cyprus provide an exceptional repository of the erosional history of Anatolia. The Kyrenia Range features several different tectonic hypotheses concerning the Eastern Mediterranean region, which are tested here using a combination of new and recently published detrital zircon geochronology, zircon trace-element data and hafnium isotopic data. Minimum detrital zircon ages refine the ages of several formations in the Kyrenia Range. The new data also provide insights into sediment provenance including far-removed sources of Upper Paleozoic zircons, within-plate versus subduction-related sources (e.g., rift; oceanic/continental arc/ophiolite) and Neogene collision-related magmatism. Facies and paleocurrent data indicate a major switch in clastic sediment input from generally southwards to westwards during the Oligocene, which was mainly controlled by the collision of the Arabian promontory with Anatolia, leaving the S Neotethys as an isolated deep-water basin.
650		4	\|a Eastern Mediterranean
650		4	\|a Kyrenia Range
650		4	\|a U-Pb zircon dating
650		4	\|a Hf isotopic analysis
650		4	\|a Sediment provenance
650		4	\|a Tectonic synthesis
700	1		\|a Robertson, Alastair H.F. \|e verfasserin \|4 aut
700	1		\|a Wu, Fu-Yuan \|e verfasserin \|4 aut
773	0	8	\|i Enthalten in \|t Earth science reviews \|d Amsterdam [u.a.] : Elsevier, 1966 \|g 233 \|h Online-Ressource \|w (DE-627)320504379 \|w (DE-600)2012642-6 \|w (DE-576)094110719 \|x 1872-6828 \|7 nnns
773	1	8	\|g volume:233
912			\|a GBV_USEFLAG_U
912			\|a SYSFLAG_U
912			\|a GBV_ELV
912			\|a SSG-OPC-GGO
912			\|a GBV_ILN_20
912			\|a GBV_ILN_22
912			\|a GBV_ILN_23
912			\|a GBV_ILN_24
912			\|a GBV_ILN_31
912			\|a GBV_ILN_32
912			\|a GBV_ILN_40
912			\|a GBV_ILN_60
912			\|a GBV_ILN_62
912			\|a GBV_ILN_63
912			\|a GBV_ILN_65
912			\|a GBV_ILN_69
912			\|a GBV_ILN_70
912			\|a GBV_ILN_73
912			\|a GBV_ILN_74
912			\|a GBV_ILN_90
912			\|a GBV_ILN_95
912			\|a GBV_ILN_100
912			\|a GBV_ILN_105
912			\|a GBV_ILN_110
912			\|a GBV_ILN_150
912			\|a GBV_ILN_151
912			\|a GBV_ILN_224
912			\|a GBV_ILN_370
912			\|a GBV_ILN_602
912			\|a GBV_ILN_702
912			\|a GBV_ILN_2003
912			\|a GBV_ILN_2004
912			\|a GBV_ILN_2005
912			\|a GBV_ILN_2011
912			\|a GBV_ILN_2014
912			\|a GBV_ILN_2015
912			\|a GBV_ILN_2020
912			\|a GBV_ILN_2021
912			\|a GBV_ILN_2025
912			\|a GBV_ILN_2027
912			\|a GBV_ILN_2034
912			\|a GBV_ILN_2038
912			\|a GBV_ILN_2044
912			\|a GBV_ILN_2048
912			\|a GBV_ILN_2049
912			\|a GBV_ILN_2050
912			\|a GBV_ILN_2056
912			\|a GBV_ILN_2059
912			\|a GBV_ILN_2061
912			\|a GBV_ILN_2064
912			\|a GBV_ILN_2065
912			\|a GBV_ILN_2068
912			\|a GBV_ILN_2111
912			\|a GBV_ILN_2112
912			\|a GBV_ILN_2113
912			\|a GBV_ILN_2118
912			\|a GBV_ILN_2122
912			\|a GBV_ILN_2129
912			\|a GBV_ILN_2143
912			\|a GBV_ILN_2147
912			\|a GBV_ILN_2148
912			\|a GBV_ILN_2152
912			\|a GBV_ILN_2153
912			\|a GBV_ILN_2190
912			\|a GBV_ILN_2336
912			\|a GBV_ILN_2507
912			\|a GBV_ILN_2522
912			\|a GBV_ILN_4035
912			\|a GBV_ILN_4037
912			\|a GBV_ILN_4112
912			\|a GBV_ILN_4125
912			\|a GBV_ILN_4126
912			\|a GBV_ILN_4242
912			\|a GBV_ILN_4251
912			\|a GBV_ILN_4305
912			\|a GBV_ILN_4313
912			\|a GBV_ILN_4323
912			\|a GBV_ILN_4324
912			\|a GBV_ILN_4326
912			\|a GBV_ILN_4333
912			\|a GBV_ILN_4334
912			\|a GBV_ILN_4335
912			\|a GBV_ILN_4338
912			\|a GBV_ILN_4393
936	b	k	\|a 38.00 \|j Geowissenschaften: Allgemeines \|q VZ
951			\|a AR
952			\|d 233

Indexfelder

author_variant	g c gc a h r ah ahr f y w fyw
matchkey_str	article:18726828:2022----::ertlicnecrnlgadeaeeiecfocatceietiteyeirnecpuipiainfrhmszicnzieo
hierarchy_sort_str	2022
bklnumber	38.00
publishDate	2022
allfields	10.1016/j.earscirev.2022.104167 doi (DE-627)ELV008571864 (ELSEVIER)S0012-8252(22)00251-3 DE-627 ger DE-627 rda eng 550 VZ 38.00 bkl Chen, Guohui verfasserin aut Detrital zircon geochronology and related evidence from clastic sediments in the Kyrenia Range, N Cyprus: Implications for the Mesozoic-Cenozoic erosional history and tectonics of southern Anatolia 2022 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Triassic to Pleistocene sandstones of the Kyrenia Range, N Cyprus provide an exceptional repository of the erosional history of Anatolia. The Kyrenia Range features several different tectonic hypotheses concerning the Eastern Mediterranean region, which are tested here using a combination of new and recently published detrital zircon geochronology, zircon trace-element data and hafnium isotopic data. Minimum detrital zircon ages refine the ages of several formations in the Kyrenia Range. The new data also provide insights into sediment provenance including far-removed sources of Upper Paleozoic zircons, within-plate versus subduction-related sources (e.g., rift; oceanic/continental arc/ophiolite) and Neogene collision-related magmatism. Facies and paleocurrent data indicate a major switch in clastic sediment input from generally southwards to westwards during the Oligocene, which was mainly controlled by the collision of the Arabian promontory with Anatolia, leaving the S Neotethys as an isolated deep-water basin. Eastern Mediterranean Kyrenia Range U-Pb zircon dating Hf isotopic analysis Sediment provenance Tectonic synthesis Robertson, Alastair H.F. verfasserin aut Wu, Fu-Yuan verfasserin aut Enthalten in Earth science reviews Amsterdam [u.a.] : Elsevier, 1966 233 Online-Ressource (DE-627)320504379 (DE-600)2012642-6 (DE-576)094110719 1872-6828 nnns volume:233 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_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.00 Geowissenschaften: Allgemeines VZ AR 233
spelling	10.1016/j.earscirev.2022.104167 doi (DE-627)ELV008571864 (ELSEVIER)S0012-8252(22)00251-3 DE-627 ger DE-627 rda eng 550 VZ 38.00 bkl Chen, Guohui verfasserin aut Detrital zircon geochronology and related evidence from clastic sediments in the Kyrenia Range, N Cyprus: Implications for the Mesozoic-Cenozoic erosional history and tectonics of southern Anatolia 2022 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Triassic to Pleistocene sandstones of the Kyrenia Range, N Cyprus provide an exceptional repository of the erosional history of Anatolia. The Kyrenia Range features several different tectonic hypotheses concerning the Eastern Mediterranean region, which are tested here using a combination of new and recently published detrital zircon geochronology, zircon trace-element data and hafnium isotopic data. Minimum detrital zircon ages refine the ages of several formations in the Kyrenia Range. The new data also provide insights into sediment provenance including far-removed sources of Upper Paleozoic zircons, within-plate versus subduction-related sources (e.g., rift; oceanic/continental arc/ophiolite) and Neogene collision-related magmatism. Facies and paleocurrent data indicate a major switch in clastic sediment input from generally southwards to westwards during the Oligocene, which was mainly controlled by the collision of the Arabian promontory with Anatolia, leaving the S Neotethys as an isolated deep-water basin. Eastern Mediterranean Kyrenia Range U-Pb zircon dating Hf isotopic analysis Sediment provenance Tectonic synthesis Robertson, Alastair H.F. verfasserin aut Wu, Fu-Yuan verfasserin aut Enthalten in Earth science reviews Amsterdam [u.a.] : Elsevier, 1966 233 Online-Ressource (DE-627)320504379 (DE-600)2012642-6 (DE-576)094110719 1872-6828 nnns volume:233 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_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.00 Geowissenschaften: Allgemeines VZ AR 233
allfields_unstemmed	10.1016/j.earscirev.2022.104167 doi (DE-627)ELV008571864 (ELSEVIER)S0012-8252(22)00251-3 DE-627 ger DE-627 rda eng 550 VZ 38.00 bkl Chen, Guohui verfasserin aut Detrital zircon geochronology and related evidence from clastic sediments in the Kyrenia Range, N Cyprus: Implications for the Mesozoic-Cenozoic erosional history and tectonics of southern Anatolia 2022 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Triassic to Pleistocene sandstones of the Kyrenia Range, N Cyprus provide an exceptional repository of the erosional history of Anatolia. The Kyrenia Range features several different tectonic hypotheses concerning the Eastern Mediterranean region, which are tested here using a combination of new and recently published detrital zircon geochronology, zircon trace-element data and hafnium isotopic data. Minimum detrital zircon ages refine the ages of several formations in the Kyrenia Range. The new data also provide insights into sediment provenance including far-removed sources of Upper Paleozoic zircons, within-plate versus subduction-related sources (e.g., rift; oceanic/continental arc/ophiolite) and Neogene collision-related magmatism. Facies and paleocurrent data indicate a major switch in clastic sediment input from generally southwards to westwards during the Oligocene, which was mainly controlled by the collision of the Arabian promontory with Anatolia, leaving the S Neotethys as an isolated deep-water basin. Eastern Mediterranean Kyrenia Range U-Pb zircon dating Hf isotopic analysis Sediment provenance Tectonic synthesis Robertson, Alastair H.F. verfasserin aut Wu, Fu-Yuan verfasserin aut Enthalten in Earth science reviews Amsterdam [u.a.] : Elsevier, 1966 233 Online-Ressource (DE-627)320504379 (DE-600)2012642-6 (DE-576)094110719 1872-6828 nnns volume:233 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_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.00 Geowissenschaften: Allgemeines VZ AR 233
allfieldsGer	10.1016/j.earscirev.2022.104167 doi (DE-627)ELV008571864 (ELSEVIER)S0012-8252(22)00251-3 DE-627 ger DE-627 rda eng 550 VZ 38.00 bkl Chen, Guohui verfasserin aut Detrital zircon geochronology and related evidence from clastic sediments in the Kyrenia Range, N Cyprus: Implications for the Mesozoic-Cenozoic erosional history and tectonics of southern Anatolia 2022 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Triassic to Pleistocene sandstones of the Kyrenia Range, N Cyprus provide an exceptional repository of the erosional history of Anatolia. The Kyrenia Range features several different tectonic hypotheses concerning the Eastern Mediterranean region, which are tested here using a combination of new and recently published detrital zircon geochronology, zircon trace-element data and hafnium isotopic data. Minimum detrital zircon ages refine the ages of several formations in the Kyrenia Range. The new data also provide insights into sediment provenance including far-removed sources of Upper Paleozoic zircons, within-plate versus subduction-related sources (e.g., rift; oceanic/continental arc/ophiolite) and Neogene collision-related magmatism. Facies and paleocurrent data indicate a major switch in clastic sediment input from generally southwards to westwards during the Oligocene, which was mainly controlled by the collision of the Arabian promontory with Anatolia, leaving the S Neotethys as an isolated deep-water basin. Eastern Mediterranean Kyrenia Range U-Pb zircon dating Hf isotopic analysis Sediment provenance Tectonic synthesis Robertson, Alastair H.F. verfasserin aut Wu, Fu-Yuan verfasserin aut Enthalten in Earth science reviews Amsterdam [u.a.] : Elsevier, 1966 233 Online-Ressource (DE-627)320504379 (DE-600)2012642-6 (DE-576)094110719 1872-6828 nnns volume:233 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_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.00 Geowissenschaften: Allgemeines VZ AR 233
allfieldsSound	10.1016/j.earscirev.2022.104167 doi (DE-627)ELV008571864 (ELSEVIER)S0012-8252(22)00251-3 DE-627 ger DE-627 rda eng 550 VZ 38.00 bkl Chen, Guohui verfasserin aut Detrital zircon geochronology and related evidence from clastic sediments in the Kyrenia Range, N Cyprus: Implications for the Mesozoic-Cenozoic erosional history and tectonics of southern Anatolia 2022 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Triassic to Pleistocene sandstones of the Kyrenia Range, N Cyprus provide an exceptional repository of the erosional history of Anatolia. The Kyrenia Range features several different tectonic hypotheses concerning the Eastern Mediterranean region, which are tested here using a combination of new and recently published detrital zircon geochronology, zircon trace-element data and hafnium isotopic data. Minimum detrital zircon ages refine the ages of several formations in the Kyrenia Range. The new data also provide insights into sediment provenance including far-removed sources of Upper Paleozoic zircons, within-plate versus subduction-related sources (e.g., rift; oceanic/continental arc/ophiolite) and Neogene collision-related magmatism. Facies and paleocurrent data indicate a major switch in clastic sediment input from generally southwards to westwards during the Oligocene, which was mainly controlled by the collision of the Arabian promontory with Anatolia, leaving the S Neotethys as an isolated deep-water basin. Eastern Mediterranean Kyrenia Range U-Pb zircon dating Hf isotopic analysis Sediment provenance Tectonic synthesis Robertson, Alastair H.F. verfasserin aut Wu, Fu-Yuan verfasserin aut Enthalten in Earth science reviews Amsterdam [u.a.] : Elsevier, 1966 233 Online-Ressource (DE-627)320504379 (DE-600)2012642-6 (DE-576)094110719 1872-6828 nnns volume:233 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_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.00 Geowissenschaften: Allgemeines VZ AR 233
language	English
source	Enthalten in Earth science reviews 233 volume:233
sourceStr	Enthalten in Earth science reviews 233 volume:233
format_phy_str_mv	Article
bklname	Geowissenschaften: Allgemeines
institution	findex.gbv.de
topic_facet	Eastern Mediterranean Kyrenia Range U-Pb zircon dating Hf isotopic analysis Sediment provenance Tectonic synthesis
dewey-raw	550
isfreeaccess_bool	false
container_title	Earth science reviews
authorswithroles_txt_mv	Chen, Guohui @@aut@@ Robertson, Alastair H.F. @@aut@@ Wu, Fu-Yuan @@aut@@
publishDateDaySort_date	2022-01-01T00:00:00Z
hierarchy_top_id	320504379
dewey-sort	3550
id	ELV008571864
language_de	englisch
fullrecord	<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">ELV008571864</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230530142410.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">230509s2022 xx \|\|\|\|\|o 00\| \|\|eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1016/j.earscirev.2022.104167</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)ELV008571864</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(ELSEVIER)S0012-8252(22)00251-3</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rda</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">38.00</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Chen, Guohui</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Detrital zircon geochronology and related evidence from clastic sediments in the Kyrenia Range, N Cyprus: Implications for the Mesozoic-Cenozoic erosional history and tectonics of southern Anatolia</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2022</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zzz</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Triassic to Pleistocene sandstones of the Kyrenia Range, N Cyprus provide an exceptional repository of the erosional history of Anatolia. The Kyrenia Range features several different tectonic hypotheses concerning the Eastern Mediterranean region, which are tested here using a combination of new and recently published detrital zircon geochronology, zircon trace-element data and hafnium isotopic data. Minimum detrital zircon ages refine the ages of several formations in the Kyrenia Range. The new data also provide insights into sediment provenance including far-removed sources of Upper Paleozoic zircons, within-plate versus subduction-related sources (e.g., rift; oceanic/continental arc/ophiolite) and Neogene collision-related magmatism. Facies and paleocurrent data indicate a major switch in clastic sediment input from generally southwards to westwards during the Oligocene, which was mainly controlled by the collision of the Arabian promontory with Anatolia, leaving the S Neotethys as an isolated deep-water basin.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Eastern Mediterranean</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Kyrenia Range</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">U-Pb zircon dating</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Hf isotopic analysis</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Sediment provenance</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Tectonic synthesis</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Robertson, Alastair H.F.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Wu, Fu-Yuan</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Earth science reviews</subfield><subfield code="d">Amsterdam [u.a.] : Elsevier, 1966</subfield><subfield code="g">233</subfield><subfield code="h">Online-Ressource</subfield><subfield code="w">(DE-627)320504379</subfield><subfield code="w">(DE-600)2012642-6</subfield><subfield code="w">(DE-576)094110719</subfield><subfield code="x">1872-6828</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:233</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ELV</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_20</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_22</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_23</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_24</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_31</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_32</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_60</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_62</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_63</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_65</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_69</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_73</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_74</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_90</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_95</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_100</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_105</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_110</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_150</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_151</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_224</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_370</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_602</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_702</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2003</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2004</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2005</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2011</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2014</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2015</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2020</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2021</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2025</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2027</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2034</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2038</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2044</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2048</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2049</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2050</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2056</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2059</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2061</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2064</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2065</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2068</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2111</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2112</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2113</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2118</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2122</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2129</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2143</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2147</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2148</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2152</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2153</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2190</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2336</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2507</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2522</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4035</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4037</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4112</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4125</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4126</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4242</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4251</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4305</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4313</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4323</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4324</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4326</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4333</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4334</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4335</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4338</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4393</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">38.00</subfield><subfield code="j">Geowissenschaften: Allgemeines</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">233</subfield></datafield></record></collection>
author	Chen, Guohui
spellingShingle	Chen, Guohui ddc 550 bkl 38.00 misc Eastern Mediterranean misc Kyrenia Range misc U-Pb zircon dating misc Hf isotopic analysis misc Sediment provenance misc Tectonic synthesis Detrital zircon geochronology and related evidence from clastic sediments in the Kyrenia Range, N Cyprus: Implications for the Mesozoic-Cenozoic erosional history and tectonics of southern Anatolia
authorStr	Chen, Guohui
ppnlink_with_tag_str_mv	@@773@@(DE-627)320504379
format	electronic Article
dewey-ones	550 - Earth sciences
delete_txt_mv	keep
author_role	aut aut aut
collection	elsevier
remote_str	true
illustrated	Not Illustrated
issn	1872-6828
topic_title	550 VZ 38.00 bkl Detrital zircon geochronology and related evidence from clastic sediments in the Kyrenia Range, N Cyprus: Implications for the Mesozoic-Cenozoic erosional history and tectonics of southern Anatolia Eastern Mediterranean Kyrenia Range U-Pb zircon dating Hf isotopic analysis Sediment provenance Tectonic synthesis
topic	ddc 550 bkl 38.00 misc Eastern Mediterranean misc Kyrenia Range misc U-Pb zircon dating misc Hf isotopic analysis misc Sediment provenance misc Tectonic synthesis
topic_unstemmed	ddc 550 bkl 38.00 misc Eastern Mediterranean misc Kyrenia Range misc U-Pb zircon dating misc Hf isotopic analysis misc Sediment provenance misc Tectonic synthesis
topic_browse	ddc 550 bkl 38.00 misc Eastern Mediterranean misc Kyrenia Range misc U-Pb zircon dating misc Hf isotopic analysis misc Sediment provenance misc Tectonic synthesis
format_facet	Elektronische Aufsätze Aufsätze Elektronische Ressource
format_main_str_mv	Text Zeitschrift/Artikel
carriertype_str_mv	cr
hierarchy_parent_title	Earth science reviews
hierarchy_parent_id	320504379
dewey-tens	550 - Earth sciences & geology
hierarchy_top_title	Earth science reviews
isfreeaccess_txt	false
familylinks_str_mv	(DE-627)320504379 (DE-600)2012642-6 (DE-576)094110719
title	Detrital zircon geochronology and related evidence from clastic sediments in the Kyrenia Range, N Cyprus: Implications for the Mesozoic-Cenozoic erosional history and tectonics of southern Anatolia
ctrlnum	(DE-627)ELV008571864 (ELSEVIER)S0012-8252(22)00251-3
title_full	Detrital zircon geochronology and related evidence from clastic sediments in the Kyrenia Range, N Cyprus: Implications for the Mesozoic-Cenozoic erosional history and tectonics of southern Anatolia
author_sort	Chen, Guohui
journal	Earth science reviews
journalStr	Earth science reviews
lang_code	eng
isOA_bool	false
dewey-hundreds	500 - Science
recordtype	marc
publishDateSort	2022
contenttype_str_mv	zzz
author_browse	Chen, Guohui Robertson, Alastair H.F. Wu, Fu-Yuan
container_volume	233
class	550 VZ 38.00 bkl
format_se	Elektronische Aufsätze
author-letter	Chen, Guohui
doi_str_mv	10.1016/j.earscirev.2022.104167
dewey-full	550
author2-role	verfasserin
title_sort	detrital zircon geochronology and related evidence from clastic sediments in the kyrenia range, n cyprus: implications for the mesozoic-cenozoic erosional history and tectonics of southern anatolia
title_auth	Detrital zircon geochronology and related evidence from clastic sediments in the Kyrenia Range, N Cyprus: Implications for the Mesozoic-Cenozoic erosional history and tectonics of southern Anatolia
abstract	Triassic to Pleistocene sandstones of the Kyrenia Range, N Cyprus provide an exceptional repository of the erosional history of Anatolia. The Kyrenia Range features several different tectonic hypotheses concerning the Eastern Mediterranean region, which are tested here using a combination of new and recently published detrital zircon geochronology, zircon trace-element data and hafnium isotopic data. Minimum detrital zircon ages refine the ages of several formations in the Kyrenia Range. The new data also provide insights into sediment provenance including far-removed sources of Upper Paleozoic zircons, within-plate versus subduction-related sources (e.g., rift; oceanic/continental arc/ophiolite) and Neogene collision-related magmatism. Facies and paleocurrent data indicate a major switch in clastic sediment input from generally southwards to westwards during the Oligocene, which was mainly controlled by the collision of the Arabian promontory with Anatolia, leaving the S Neotethys as an isolated deep-water basin.
abstractGer	Triassic to Pleistocene sandstones of the Kyrenia Range, N Cyprus provide an exceptional repository of the erosional history of Anatolia. The Kyrenia Range features several different tectonic hypotheses concerning the Eastern Mediterranean region, which are tested here using a combination of new and recently published detrital zircon geochronology, zircon trace-element data and hafnium isotopic data. Minimum detrital zircon ages refine the ages of several formations in the Kyrenia Range. The new data also provide insights into sediment provenance including far-removed sources of Upper Paleozoic zircons, within-plate versus subduction-related sources (e.g., rift; oceanic/continental arc/ophiolite) and Neogene collision-related magmatism. Facies and paleocurrent data indicate a major switch in clastic sediment input from generally southwards to westwards during the Oligocene, which was mainly controlled by the collision of the Arabian promontory with Anatolia, leaving the S Neotethys as an isolated deep-water basin.
abstract_unstemmed	Triassic to Pleistocene sandstones of the Kyrenia Range, N Cyprus provide an exceptional repository of the erosional history of Anatolia. The Kyrenia Range features several different tectonic hypotheses concerning the Eastern Mediterranean region, which are tested here using a combination of new and recently published detrital zircon geochronology, zircon trace-element data and hafnium isotopic data. Minimum detrital zircon ages refine the ages of several formations in the Kyrenia Range. The new data also provide insights into sediment provenance including far-removed sources of Upper Paleozoic zircons, within-plate versus subduction-related sources (e.g., rift; oceanic/continental arc/ophiolite) and Neogene collision-related magmatism. Facies and paleocurrent data indicate a major switch in clastic sediment input from generally southwards to westwards during the Oligocene, which was mainly controlled by the collision of the Arabian promontory with Anatolia, leaving the S Neotethys as an isolated deep-water basin.
collection_details	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_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393
title_short	Detrital zircon geochronology and related evidence from clastic sediments in the Kyrenia Range, N Cyprus: Implications for the Mesozoic-Cenozoic erosional history and tectonics of southern Anatolia
remote_bool	true
author2	Robertson, Alastair H.F. Wu, Fu-Yuan
author2Str	Robertson, Alastair H.F. Wu, Fu-Yuan
ppnlink	320504379
mediatype_str_mv	c
isOA_txt	false
hochschulschrift_bool	false
doi_str	10.1016/j.earscirev.2022.104167
up_date	2024-07-06T20:09:35.589Z
_version_	1803861702046908416
fullrecord_marcxml	<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">ELV008571864</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230530142410.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">230509s2022 xx \|\|\|\|\|o 00\| \|\|eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1016/j.earscirev.2022.104167</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)ELV008571864</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(ELSEVIER)S0012-8252(22)00251-3</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rda</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">38.00</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Chen, Guohui</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Detrital zircon geochronology and related evidence from clastic sediments in the Kyrenia Range, N Cyprus: Implications for the Mesozoic-Cenozoic erosional history and tectonics of southern Anatolia</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2022</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zzz</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Triassic to Pleistocene sandstones of the Kyrenia Range, N Cyprus provide an exceptional repository of the erosional history of Anatolia. The Kyrenia Range features several different tectonic hypotheses concerning the Eastern Mediterranean region, which are tested here using a combination of new and recently published detrital zircon geochronology, zircon trace-element data and hafnium isotopic data. Minimum detrital zircon ages refine the ages of several formations in the Kyrenia Range. The new data also provide insights into sediment provenance including far-removed sources of Upper Paleozoic zircons, within-plate versus subduction-related sources (e.g., rift; oceanic/continental arc/ophiolite) and Neogene collision-related magmatism. Facies and paleocurrent data indicate a major switch in clastic sediment input from generally southwards to westwards during the Oligocene, which was mainly controlled by the collision of the Arabian promontory with Anatolia, leaving the S Neotethys as an isolated deep-water basin.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Eastern Mediterranean</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Kyrenia Range</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">U-Pb zircon dating</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Hf isotopic analysis</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Sediment provenance</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Tectonic synthesis</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Robertson, Alastair H.F.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Wu, Fu-Yuan</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Earth science reviews</subfield><subfield code="d">Amsterdam [u.a.] : Elsevier, 1966</subfield><subfield code="g">233</subfield><subfield code="h">Online-Ressource</subfield><subfield code="w">(DE-627)320504379</subfield><subfield code="w">(DE-600)2012642-6</subfield><subfield code="w">(DE-576)094110719</subfield><subfield code="x">1872-6828</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:233</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ELV</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_20</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_22</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_23</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_24</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_31</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_32</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_60</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_62</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_63</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_65</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_69</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_73</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_74</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_90</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_95</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_100</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_105</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_110</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_150</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_151</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_224</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_370</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_602</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_702</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2003</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2004</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2005</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2011</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2014</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2015</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2020</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2021</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2025</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2027</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2034</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2038</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2044</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2048</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2049</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2050</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2056</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2059</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2061</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2064</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2065</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2068</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2111</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2112</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2113</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2118</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2122</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2129</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2143</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2147</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2148</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2152</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2153</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2190</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2336</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2507</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2522</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4035</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4037</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4112</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4125</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4126</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4242</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4251</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4305</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4313</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4323</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4324</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4326</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4333</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4334</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4335</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4338</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4393</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">38.00</subfield><subfield code="j">Geowissenschaften: Allgemeines</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">233</subfield></datafield></record></collection>
score	7.400714

Nicht das Richtige dabei?

Schreiben Sie uns!

Detrital zircon geochronology and related evidence from clastic sediments in the Kyrenia Range, N Cyprus: Implications for the Mesozoic-Cenozoic erosional history and tectonics of southern Anatolia

Nicht das Richtige dabei?

Zugang & Verfügbarkeit

Vorhandene Bände

Nicht das Richtige dabei?