Factors controlling carbonate slope failures: Insight from stratigraphic forward modelling

A carbonate slope links platform and basin-floor regions holding crucial information on the carbonate source-sink system of a vast ocean. There is a generally poor understanding of the entire process of carbonate slope deposition, failure, and subsequent transportation and redeposition etc. due to the lack of field observation and adequate numerical modelling algorithms. Based on a comprehensive literature review on carbonate slope failures, a three-segment carbonate slope depositional model was conceptualized and simulated using a stratigraphic forward modelling (SFM) program. The model is capable of simulating carbonate slope failures in a) subaerial, b) shallow marine, and c) deep marine settings concurrently. The SFM program was employed to simulate the evolution of carbonate slope and the occurrence and distribution of mass transport deposits (MTDs) in a deeply buried upper Ediacaran carbonate succession in the central Sichuan Basin, China. The simulation results show that MTDs were mainly developed at the toe-of-slopes and in the center of the Ediacaran trough, offering a new potential play for future hydrocarbon exploration in the area. Several key factors controlling carbonate slope failures, including carbonate lithologies, carbonate growth rates, and frequencies and amplitudes of sea-level fluctuations, were quantitatively evaluated in both time and space domains. Simulations have confirmed that carbonate lithologies can notably affect the frequency and magnitude of slope failures and the development of MTDs, indicating that the higher the proportions of coarser and cemented sediments, the less frequent slope failures and the less the volume of the MTDs would be. The frequency of slope failures and the volume of the MTDs would increase with carbonate growth rates. Slope failures are more likely to be triggered by high-frequency sea-level fluctuations than by low-frequency sea-level changes. For a given sea-level change frequency, the magnitude of a single slope failure event and the total volume of associated MTDs are more likely to be more significant under a greenhouse climate, with a relatively smaller amplitude of sea-level changes, than under an icehouse climate. Ausführliche Beschreibung

Gespeichert in:

Autor*in:	Liu, Jianliang [verfasserIn] Liu, Keyu [verfasserIn] Salles, Tristan [verfasserIn] Li, Changwei [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2022

Schlagwörter:	Carbonate slope failure Mass transport deposits Tectono-sedimentary evolution Controlling factors Stratigraphic forward modelling Sichuan Basin

Übergeordnetes Werk:	Enthalten in: Earth science reviews - Amsterdam [u.a.] : Elsevier, 1966, 232
Übergeordnetes Werk:	volume:232

DOI / URN:	10.1016/j.earscirev.2022.104108

Katalog-ID:	ELV008494851

Internformat


LEADER	01000caa a22002652 4500
001	ELV008494851
003	DE-627
005	20230524152428.0
007	cr uuu---uuuuu
008	230509s2022 xx \|\|\|\|\|o 00\| \|\|eng c
024	7		\|a 10.1016/j.earscirev.2022.104108 \|2 doi
035			\|a (DE-627)ELV008494851
035			\|a (ELSEVIER)S0012-8252(22)00192-1
040			\|a DE-627 \|b ger \|c DE-627 \|e rda
041			\|a eng
082	0	4	\|a 550 \|q DE-600
084			\|a 38.00 \|2 bkl
100	1		\|a Liu, Jianliang \|e verfasserin \|4 aut
245	1	0	\|a Factors controlling carbonate slope failures: Insight from stratigraphic forward modelling
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 A carbonate slope links platform and basin-floor regions holding crucial information on the carbonate source-sink system of a vast ocean. There is a generally poor understanding of the entire process of carbonate slope deposition, failure, and subsequent transportation and redeposition etc. due to the lack of field observation and adequate numerical modelling algorithms. Based on a comprehensive literature review on carbonate slope failures, a three-segment carbonate slope depositional model was conceptualized and simulated using a stratigraphic forward modelling (SFM) program. The model is capable of simulating carbonate slope failures in a) subaerial, b) shallow marine, and c) deep marine settings concurrently. The SFM program was employed to simulate the evolution of carbonate slope and the occurrence and distribution of mass transport deposits (MTDs) in a deeply buried upper Ediacaran carbonate succession in the central Sichuan Basin, China. The simulation results show that MTDs were mainly developed at the toe-of-slopes and in the center of the Ediacaran trough, offering a new potential play for future hydrocarbon exploration in the area. Several key factors controlling carbonate slope failures, including carbonate lithologies, carbonate growth rates, and frequencies and amplitudes of sea-level fluctuations, were quantitatively evaluated in both time and space domains. Simulations have confirmed that carbonate lithologies can notably affect the frequency and magnitude of slope failures and the development of MTDs, indicating that the higher the proportions of coarser and cemented sediments, the less frequent slope failures and the less the volume of the MTDs would be. The frequency of slope failures and the volume of the MTDs would increase with carbonate growth rates. Slope failures are more likely to be triggered by high-frequency sea-level fluctuations than by low-frequency sea-level changes. For a given sea-level change frequency, the magnitude of a single slope failure event and the total volume of associated MTDs are more likely to be more significant under a greenhouse climate, with a relatively smaller amplitude of sea-level changes, than under an icehouse climate.
650		4	\|a Carbonate slope failure
650		4	\|a Mass transport deposits
650		4	\|a Tectono-sedimentary evolution
650		4	\|a Controlling factors
650		4	\|a Stratigraphic forward modelling
650		4	\|a Sichuan Basin
700	1		\|a Liu, Keyu \|e verfasserin \|4 aut
700	1		\|a Salles, Tristan \|e verfasserin \|4 aut
700	1		\|a Li, Changwei \|e verfasserin \|4 aut
773	0	8	\|i Enthalten in \|t Earth science reviews \|d Amsterdam [u.a.] : Elsevier, 1966 \|g 232 \|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:232
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
951			\|a AR
952			\|d 232

Indexfelder

author_variant	j l jl k l kl t s ts c l cl
matchkey_str	article:18726828:2022----::atrcnrligabntsoealrsnihfosrtga
hierarchy_sort_str	2022
bklnumber	38.00
publishDate	2022
allfields	10.1016/j.earscirev.2022.104108 doi (DE-627)ELV008494851 (ELSEVIER)S0012-8252(22)00192-1 DE-627 ger DE-627 rda eng 550 DE-600 38.00 bkl Liu, Jianliang verfasserin aut Factors controlling carbonate slope failures: Insight from stratigraphic forward modelling 2022 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier A carbonate slope links platform and basin-floor regions holding crucial information on the carbonate source-sink system of a vast ocean. There is a generally poor understanding of the entire process of carbonate slope deposition, failure, and subsequent transportation and redeposition etc. due to the lack of field observation and adequate numerical modelling algorithms. Based on a comprehensive literature review on carbonate slope failures, a three-segment carbonate slope depositional model was conceptualized and simulated using a stratigraphic forward modelling (SFM) program. The model is capable of simulating carbonate slope failures in a) subaerial, b) shallow marine, and c) deep marine settings concurrently. The SFM program was employed to simulate the evolution of carbonate slope and the occurrence and distribution of mass transport deposits (MTDs) in a deeply buried upper Ediacaran carbonate succession in the central Sichuan Basin, China. The simulation results show that MTDs were mainly developed at the toe-of-slopes and in the center of the Ediacaran trough, offering a new potential play for future hydrocarbon exploration in the area. Several key factors controlling carbonate slope failures, including carbonate lithologies, carbonate growth rates, and frequencies and amplitudes of sea-level fluctuations, were quantitatively evaluated in both time and space domains. Simulations have confirmed that carbonate lithologies can notably affect the frequency and magnitude of slope failures and the development of MTDs, indicating that the higher the proportions of coarser and cemented sediments, the less frequent slope failures and the less the volume of the MTDs would be. The frequency of slope failures and the volume of the MTDs would increase with carbonate growth rates. Slope failures are more likely to be triggered by high-frequency sea-level fluctuations than by low-frequency sea-level changes. For a given sea-level change frequency, the magnitude of a single slope failure event and the total volume of associated MTDs are more likely to be more significant under a greenhouse climate, with a relatively smaller amplitude of sea-level changes, than under an icehouse climate. Carbonate slope failure Mass transport deposits Tectono-sedimentary evolution Controlling factors Stratigraphic forward modelling Sichuan Basin Liu, Keyu verfasserin aut Salles, Tristan verfasserin aut Li, Changwei verfasserin aut Enthalten in Earth science reviews Amsterdam [u.a.] : Elsevier, 1966 232 Online-Ressource (DE-627)320504379 (DE-600)2012642-6 (DE-576)094110719 1872-6828 nnns volume:232 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 AR 232
spelling	10.1016/j.earscirev.2022.104108 doi (DE-627)ELV008494851 (ELSEVIER)S0012-8252(22)00192-1 DE-627 ger DE-627 rda eng 550 DE-600 38.00 bkl Liu, Jianliang verfasserin aut Factors controlling carbonate slope failures: Insight from stratigraphic forward modelling 2022 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier A carbonate slope links platform and basin-floor regions holding crucial information on the carbonate source-sink system of a vast ocean. There is a generally poor understanding of the entire process of carbonate slope deposition, failure, and subsequent transportation and redeposition etc. due to the lack of field observation and adequate numerical modelling algorithms. Based on a comprehensive literature review on carbonate slope failures, a three-segment carbonate slope depositional model was conceptualized and simulated using a stratigraphic forward modelling (SFM) program. The model is capable of simulating carbonate slope failures in a) subaerial, b) shallow marine, and c) deep marine settings concurrently. The SFM program was employed to simulate the evolution of carbonate slope and the occurrence and distribution of mass transport deposits (MTDs) in a deeply buried upper Ediacaran carbonate succession in the central Sichuan Basin, China. The simulation results show that MTDs were mainly developed at the toe-of-slopes and in the center of the Ediacaran trough, offering a new potential play for future hydrocarbon exploration in the area. Several key factors controlling carbonate slope failures, including carbonate lithologies, carbonate growth rates, and frequencies and amplitudes of sea-level fluctuations, were quantitatively evaluated in both time and space domains. Simulations have confirmed that carbonate lithologies can notably affect the frequency and magnitude of slope failures and the development of MTDs, indicating that the higher the proportions of coarser and cemented sediments, the less frequent slope failures and the less the volume of the MTDs would be. The frequency of slope failures and the volume of the MTDs would increase with carbonate growth rates. Slope failures are more likely to be triggered by high-frequency sea-level fluctuations than by low-frequency sea-level changes. For a given sea-level change frequency, the magnitude of a single slope failure event and the total volume of associated MTDs are more likely to be more significant under a greenhouse climate, with a relatively smaller amplitude of sea-level changes, than under an icehouse climate. Carbonate slope failure Mass transport deposits Tectono-sedimentary evolution Controlling factors Stratigraphic forward modelling Sichuan Basin Liu, Keyu verfasserin aut Salles, Tristan verfasserin aut Li, Changwei verfasserin aut Enthalten in Earth science reviews Amsterdam [u.a.] : Elsevier, 1966 232 Online-Ressource (DE-627)320504379 (DE-600)2012642-6 (DE-576)094110719 1872-6828 nnns volume:232 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 AR 232
allfields_unstemmed	10.1016/j.earscirev.2022.104108 doi (DE-627)ELV008494851 (ELSEVIER)S0012-8252(22)00192-1 DE-627 ger DE-627 rda eng 550 DE-600 38.00 bkl Liu, Jianliang verfasserin aut Factors controlling carbonate slope failures: Insight from stratigraphic forward modelling 2022 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier A carbonate slope links platform and basin-floor regions holding crucial information on the carbonate source-sink system of a vast ocean. There is a generally poor understanding of the entire process of carbonate slope deposition, failure, and subsequent transportation and redeposition etc. due to the lack of field observation and adequate numerical modelling algorithms. Based on a comprehensive literature review on carbonate slope failures, a three-segment carbonate slope depositional model was conceptualized and simulated using a stratigraphic forward modelling (SFM) program. The model is capable of simulating carbonate slope failures in a) subaerial, b) shallow marine, and c) deep marine settings concurrently. The SFM program was employed to simulate the evolution of carbonate slope and the occurrence and distribution of mass transport deposits (MTDs) in a deeply buried upper Ediacaran carbonate succession in the central Sichuan Basin, China. The simulation results show that MTDs were mainly developed at the toe-of-slopes and in the center of the Ediacaran trough, offering a new potential play for future hydrocarbon exploration in the area. Several key factors controlling carbonate slope failures, including carbonate lithologies, carbonate growth rates, and frequencies and amplitudes of sea-level fluctuations, were quantitatively evaluated in both time and space domains. Simulations have confirmed that carbonate lithologies can notably affect the frequency and magnitude of slope failures and the development of MTDs, indicating that the higher the proportions of coarser and cemented sediments, the less frequent slope failures and the less the volume of the MTDs would be. The frequency of slope failures and the volume of the MTDs would increase with carbonate growth rates. Slope failures are more likely to be triggered by high-frequency sea-level fluctuations than by low-frequency sea-level changes. For a given sea-level change frequency, the magnitude of a single slope failure event and the total volume of associated MTDs are more likely to be more significant under a greenhouse climate, with a relatively smaller amplitude of sea-level changes, than under an icehouse climate. Carbonate slope failure Mass transport deposits Tectono-sedimentary evolution Controlling factors Stratigraphic forward modelling Sichuan Basin Liu, Keyu verfasserin aut Salles, Tristan verfasserin aut Li, Changwei verfasserin aut Enthalten in Earth science reviews Amsterdam [u.a.] : Elsevier, 1966 232 Online-Ressource (DE-627)320504379 (DE-600)2012642-6 (DE-576)094110719 1872-6828 nnns volume:232 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 AR 232
allfieldsGer	10.1016/j.earscirev.2022.104108 doi (DE-627)ELV008494851 (ELSEVIER)S0012-8252(22)00192-1 DE-627 ger DE-627 rda eng 550 DE-600 38.00 bkl Liu, Jianliang verfasserin aut Factors controlling carbonate slope failures: Insight from stratigraphic forward modelling 2022 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier A carbonate slope links platform and basin-floor regions holding crucial information on the carbonate source-sink system of a vast ocean. There is a generally poor understanding of the entire process of carbonate slope deposition, failure, and subsequent transportation and redeposition etc. due to the lack of field observation and adequate numerical modelling algorithms. Based on a comprehensive literature review on carbonate slope failures, a three-segment carbonate slope depositional model was conceptualized and simulated using a stratigraphic forward modelling (SFM) program. The model is capable of simulating carbonate slope failures in a) subaerial, b) shallow marine, and c) deep marine settings concurrently. The SFM program was employed to simulate the evolution of carbonate slope and the occurrence and distribution of mass transport deposits (MTDs) in a deeply buried upper Ediacaran carbonate succession in the central Sichuan Basin, China. The simulation results show that MTDs were mainly developed at the toe-of-slopes and in the center of the Ediacaran trough, offering a new potential play for future hydrocarbon exploration in the area. Several key factors controlling carbonate slope failures, including carbonate lithologies, carbonate growth rates, and frequencies and amplitudes of sea-level fluctuations, were quantitatively evaluated in both time and space domains. Simulations have confirmed that carbonate lithologies can notably affect the frequency and magnitude of slope failures and the development of MTDs, indicating that the higher the proportions of coarser and cemented sediments, the less frequent slope failures and the less the volume of the MTDs would be. The frequency of slope failures and the volume of the MTDs would increase with carbonate growth rates. Slope failures are more likely to be triggered by high-frequency sea-level fluctuations than by low-frequency sea-level changes. For a given sea-level change frequency, the magnitude of a single slope failure event and the total volume of associated MTDs are more likely to be more significant under a greenhouse climate, with a relatively smaller amplitude of sea-level changes, than under an icehouse climate. Carbonate slope failure Mass transport deposits Tectono-sedimentary evolution Controlling factors Stratigraphic forward modelling Sichuan Basin Liu, Keyu verfasserin aut Salles, Tristan verfasserin aut Li, Changwei verfasserin aut Enthalten in Earth science reviews Amsterdam [u.a.] : Elsevier, 1966 232 Online-Ressource (DE-627)320504379 (DE-600)2012642-6 (DE-576)094110719 1872-6828 nnns volume:232 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 AR 232
allfieldsSound	10.1016/j.earscirev.2022.104108 doi (DE-627)ELV008494851 (ELSEVIER)S0012-8252(22)00192-1 DE-627 ger DE-627 rda eng 550 DE-600 38.00 bkl Liu, Jianliang verfasserin aut Factors controlling carbonate slope failures: Insight from stratigraphic forward modelling 2022 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier A carbonate slope links platform and basin-floor regions holding crucial information on the carbonate source-sink system of a vast ocean. There is a generally poor understanding of the entire process of carbonate slope deposition, failure, and subsequent transportation and redeposition etc. due to the lack of field observation and adequate numerical modelling algorithms. Based on a comprehensive literature review on carbonate slope failures, a three-segment carbonate slope depositional model was conceptualized and simulated using a stratigraphic forward modelling (SFM) program. The model is capable of simulating carbonate slope failures in a) subaerial, b) shallow marine, and c) deep marine settings concurrently. The SFM program was employed to simulate the evolution of carbonate slope and the occurrence and distribution of mass transport deposits (MTDs) in a deeply buried upper Ediacaran carbonate succession in the central Sichuan Basin, China. The simulation results show that MTDs were mainly developed at the toe-of-slopes and in the center of the Ediacaran trough, offering a new potential play for future hydrocarbon exploration in the area. Several key factors controlling carbonate slope failures, including carbonate lithologies, carbonate growth rates, and frequencies and amplitudes of sea-level fluctuations, were quantitatively evaluated in both time and space domains. Simulations have confirmed that carbonate lithologies can notably affect the frequency and magnitude of slope failures and the development of MTDs, indicating that the higher the proportions of coarser and cemented sediments, the less frequent slope failures and the less the volume of the MTDs would be. The frequency of slope failures and the volume of the MTDs would increase with carbonate growth rates. Slope failures are more likely to be triggered by high-frequency sea-level fluctuations than by low-frequency sea-level changes. For a given sea-level change frequency, the magnitude of a single slope failure event and the total volume of associated MTDs are more likely to be more significant under a greenhouse climate, with a relatively smaller amplitude of sea-level changes, than under an icehouse climate. Carbonate slope failure Mass transport deposits Tectono-sedimentary evolution Controlling factors Stratigraphic forward modelling Sichuan Basin Liu, Keyu verfasserin aut Salles, Tristan verfasserin aut Li, Changwei verfasserin aut Enthalten in Earth science reviews Amsterdam [u.a.] : Elsevier, 1966 232 Online-Ressource (DE-627)320504379 (DE-600)2012642-6 (DE-576)094110719 1872-6828 nnns volume:232 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 AR 232
language	English
source	Enthalten in Earth science reviews 232 volume:232
sourceStr	Enthalten in Earth science reviews 232 volume:232
format_phy_str_mv	Article
bklname	Geowissenschaften: Allgemeines
institution	findex.gbv.de
topic_facet	Carbonate slope failure Mass transport deposits Tectono-sedimentary evolution Controlling factors Stratigraphic forward modelling Sichuan Basin
dewey-raw	550
isfreeaccess_bool	false
container_title	Earth science reviews
authorswithroles_txt_mv	Liu, Jianliang @@aut@@ Liu, Keyu @@aut@@ Salles, Tristan @@aut@@ Li, Changwei @@aut@@
publishDateDaySort_date	2022-01-01T00:00:00Z
hierarchy_top_id	320504379
dewey-sort	3550
id	ELV008494851
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">ELV008494851</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230524152428.0</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.2022.104108</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)ELV008494851</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(ELSEVIER)S0012-8252(22)00192-1</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">DE-600</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">Liu, Jianliang</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Factors controlling carbonate slope failures: Insight from stratigraphic forward modelling</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">A carbonate slope links platform and basin-floor regions holding crucial information on the carbonate source-sink system of a vast ocean. There is a generally poor understanding of the entire process of carbonate slope deposition, failure, and subsequent transportation and redeposition etc. due to the lack of field observation and adequate numerical modelling algorithms. Based on a comprehensive literature review on carbonate slope failures, a three-segment carbonate slope depositional model was conceptualized and simulated using a stratigraphic forward modelling (SFM) program. The model is capable of simulating carbonate slope failures in a) subaerial, b) shallow marine, and c) deep marine settings concurrently. The SFM program was employed to simulate the evolution of carbonate slope and the occurrence and distribution of mass transport deposits (MTDs) in a deeply buried upper Ediacaran carbonate succession in the central Sichuan Basin, China. The simulation results show that MTDs were mainly developed at the toe-of-slopes and in the center of the Ediacaran trough, offering a new potential play for future hydrocarbon exploration in the area. Several key factors controlling carbonate slope failures, including carbonate lithologies, carbonate growth rates, and frequencies and amplitudes of sea-level fluctuations, were quantitatively evaluated in both time and space domains. Simulations have confirmed that carbonate lithologies can notably affect the frequency and magnitude of slope failures and the development of MTDs, indicating that the higher the proportions of coarser and cemented sediments, the less frequent slope failures and the less the volume of the MTDs would be. The frequency of slope failures and the volume of the MTDs would increase with carbonate growth rates. Slope failures are more likely to be triggered by high-frequency sea-level fluctuations than by low-frequency sea-level changes. For a given sea-level change frequency, the magnitude of a single slope failure event and the total volume of associated MTDs are more likely to be more significant under a greenhouse climate, with a relatively smaller amplitude of sea-level changes, than under an icehouse climate.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Carbonate slope failure</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Mass transport deposits</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Tectono-sedimentary evolution</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Controlling factors</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Stratigraphic forward modelling</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Sichuan Basin</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Liu, Keyu</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Salles, Tristan</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Li, Changwei</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">232</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:232</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></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">232</subfield></datafield></record></collection>
author	Liu, Jianliang
spellingShingle	Liu, Jianliang ddc 550 bkl 38.00 misc Carbonate slope failure misc Mass transport deposits misc Tectono-sedimentary evolution misc Controlling factors misc Stratigraphic forward modelling misc Sichuan Basin Factors controlling carbonate slope failures: Insight from stratigraphic forward modelling
authorStr	Liu, Jianliang
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 aut
collection	elsevier
remote_str	true
illustrated	Not Illustrated
issn	1872-6828
topic_title	550 DE-600 38.00 bkl Factors controlling carbonate slope failures: Insight from stratigraphic forward modelling Carbonate slope failure Mass transport deposits Tectono-sedimentary evolution Controlling factors Stratigraphic forward modelling Sichuan Basin
topic	ddc 550 bkl 38.00 misc Carbonate slope failure misc Mass transport deposits misc Tectono-sedimentary evolution misc Controlling factors misc Stratigraphic forward modelling misc Sichuan Basin
topic_unstemmed	ddc 550 bkl 38.00 misc Carbonate slope failure misc Mass transport deposits misc Tectono-sedimentary evolution misc Controlling factors misc Stratigraphic forward modelling misc Sichuan Basin
topic_browse	ddc 550 bkl 38.00 misc Carbonate slope failure misc Mass transport deposits misc Tectono-sedimentary evolution misc Controlling factors misc Stratigraphic forward modelling misc Sichuan Basin
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	Factors controlling carbonate slope failures: Insight from stratigraphic forward modelling
ctrlnum	(DE-627)ELV008494851 (ELSEVIER)S0012-8252(22)00192-1
title_full	Factors controlling carbonate slope failures: Insight from stratigraphic forward modelling
author_sort	Liu, Jianliang
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	Liu, Jianliang Liu, Keyu Salles, Tristan Li, Changwei
container_volume	232
class	550 DE-600 38.00 bkl
format_se	Elektronische Aufsätze
author-letter	Liu, Jianliang
doi_str_mv	10.1016/j.earscirev.2022.104108
dewey-full	550
author2-role	verfasserin
title_sort	factors controlling carbonate slope failures: insight from stratigraphic forward modelling
title_auth	Factors controlling carbonate slope failures: Insight from stratigraphic forward modelling
abstract	A carbonate slope links platform and basin-floor regions holding crucial information on the carbonate source-sink system of a vast ocean. There is a generally poor understanding of the entire process of carbonate slope deposition, failure, and subsequent transportation and redeposition etc. due to the lack of field observation and adequate numerical modelling algorithms. Based on a comprehensive literature review on carbonate slope failures, a three-segment carbonate slope depositional model was conceptualized and simulated using a stratigraphic forward modelling (SFM) program. The model is capable of simulating carbonate slope failures in a) subaerial, b) shallow marine, and c) deep marine settings concurrently. The SFM program was employed to simulate the evolution of carbonate slope and the occurrence and distribution of mass transport deposits (MTDs) in a deeply buried upper Ediacaran carbonate succession in the central Sichuan Basin, China. The simulation results show that MTDs were mainly developed at the toe-of-slopes and in the center of the Ediacaran trough, offering a new potential play for future hydrocarbon exploration in the area. Several key factors controlling carbonate slope failures, including carbonate lithologies, carbonate growth rates, and frequencies and amplitudes of sea-level fluctuations, were quantitatively evaluated in both time and space domains. Simulations have confirmed that carbonate lithologies can notably affect the frequency and magnitude of slope failures and the development of MTDs, indicating that the higher the proportions of coarser and cemented sediments, the less frequent slope failures and the less the volume of the MTDs would be. The frequency of slope failures and the volume of the MTDs would increase with carbonate growth rates. Slope failures are more likely to be triggered by high-frequency sea-level fluctuations than by low-frequency sea-level changes. For a given sea-level change frequency, the magnitude of a single slope failure event and the total volume of associated MTDs are more likely to be more significant under a greenhouse climate, with a relatively smaller amplitude of sea-level changes, than under an icehouse climate.
abstractGer	A carbonate slope links platform and basin-floor regions holding crucial information on the carbonate source-sink system of a vast ocean. There is a generally poor understanding of the entire process of carbonate slope deposition, failure, and subsequent transportation and redeposition etc. due to the lack of field observation and adequate numerical modelling algorithms. Based on a comprehensive literature review on carbonate slope failures, a three-segment carbonate slope depositional model was conceptualized and simulated using a stratigraphic forward modelling (SFM) program. The model is capable of simulating carbonate slope failures in a) subaerial, b) shallow marine, and c) deep marine settings concurrently. The SFM program was employed to simulate the evolution of carbonate slope and the occurrence and distribution of mass transport deposits (MTDs) in a deeply buried upper Ediacaran carbonate succession in the central Sichuan Basin, China. The simulation results show that MTDs were mainly developed at the toe-of-slopes and in the center of the Ediacaran trough, offering a new potential play for future hydrocarbon exploration in the area. Several key factors controlling carbonate slope failures, including carbonate lithologies, carbonate growth rates, and frequencies and amplitudes of sea-level fluctuations, were quantitatively evaluated in both time and space domains. Simulations have confirmed that carbonate lithologies can notably affect the frequency and magnitude of slope failures and the development of MTDs, indicating that the higher the proportions of coarser and cemented sediments, the less frequent slope failures and the less the volume of the MTDs would be. The frequency of slope failures and the volume of the MTDs would increase with carbonate growth rates. Slope failures are more likely to be triggered by high-frequency sea-level fluctuations than by low-frequency sea-level changes. For a given sea-level change frequency, the magnitude of a single slope failure event and the total volume of associated MTDs are more likely to be more significant under a greenhouse climate, with a relatively smaller amplitude of sea-level changes, than under an icehouse climate.
abstract_unstemmed	A carbonate slope links platform and basin-floor regions holding crucial information on the carbonate source-sink system of a vast ocean. There is a generally poor understanding of the entire process of carbonate slope deposition, failure, and subsequent transportation and redeposition etc. due to the lack of field observation and adequate numerical modelling algorithms. Based on a comprehensive literature review on carbonate slope failures, a three-segment carbonate slope depositional model was conceptualized and simulated using a stratigraphic forward modelling (SFM) program. The model is capable of simulating carbonate slope failures in a) subaerial, b) shallow marine, and c) deep marine settings concurrently. The SFM program was employed to simulate the evolution of carbonate slope and the occurrence and distribution of mass transport deposits (MTDs) in a deeply buried upper Ediacaran carbonate succession in the central Sichuan Basin, China. The simulation results show that MTDs were mainly developed at the toe-of-slopes and in the center of the Ediacaran trough, offering a new potential play for future hydrocarbon exploration in the area. Several key factors controlling carbonate slope failures, including carbonate lithologies, carbonate growth rates, and frequencies and amplitudes of sea-level fluctuations, were quantitatively evaluated in both time and space domains. Simulations have confirmed that carbonate lithologies can notably affect the frequency and magnitude of slope failures and the development of MTDs, indicating that the higher the proportions of coarser and cemented sediments, the less frequent slope failures and the less the volume of the MTDs would be. The frequency of slope failures and the volume of the MTDs would increase with carbonate growth rates. Slope failures are more likely to be triggered by high-frequency sea-level fluctuations than by low-frequency sea-level changes. For a given sea-level change frequency, the magnitude of a single slope failure event and the total volume of associated MTDs are more likely to be more significant under a greenhouse climate, with a relatively smaller amplitude of sea-level changes, than under an icehouse climate.
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	Factors controlling carbonate slope failures: Insight from stratigraphic forward modelling
remote_bool	true
author2	Liu, Keyu Salles, Tristan Li, Changwei
author2Str	Liu, Keyu Salles, Tristan Li, Changwei
ppnlink	320504379
mediatype_str_mv	c
isOA_txt	false
hochschulschrift_bool	false
doi_str	10.1016/j.earscirev.2022.104108
up_date	2024-07-06T19:53:41.555Z
_version_	1803860701669752832
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">ELV008494851</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230524152428.0</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.2022.104108</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)ELV008494851</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(ELSEVIER)S0012-8252(22)00192-1</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">DE-600</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">Liu, Jianliang</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Factors controlling carbonate slope failures: Insight from stratigraphic forward modelling</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">A carbonate slope links platform and basin-floor regions holding crucial information on the carbonate source-sink system of a vast ocean. There is a generally poor understanding of the entire process of carbonate slope deposition, failure, and subsequent transportation and redeposition etc. due to the lack of field observation and adequate numerical modelling algorithms. Based on a comprehensive literature review on carbonate slope failures, a three-segment carbonate slope depositional model was conceptualized and simulated using a stratigraphic forward modelling (SFM) program. The model is capable of simulating carbonate slope failures in a) subaerial, b) shallow marine, and c) deep marine settings concurrently. The SFM program was employed to simulate the evolution of carbonate slope and the occurrence and distribution of mass transport deposits (MTDs) in a deeply buried upper Ediacaran carbonate succession in the central Sichuan Basin, China. The simulation results show that MTDs were mainly developed at the toe-of-slopes and in the center of the Ediacaran trough, offering a new potential play for future hydrocarbon exploration in the area. Several key factors controlling carbonate slope failures, including carbonate lithologies, carbonate growth rates, and frequencies and amplitudes of sea-level fluctuations, were quantitatively evaluated in both time and space domains. Simulations have confirmed that carbonate lithologies can notably affect the frequency and magnitude of slope failures and the development of MTDs, indicating that the higher the proportions of coarser and cemented sediments, the less frequent slope failures and the less the volume of the MTDs would be. The frequency of slope failures and the volume of the MTDs would increase with carbonate growth rates. Slope failures are more likely to be triggered by high-frequency sea-level fluctuations than by low-frequency sea-level changes. For a given sea-level change frequency, the magnitude of a single slope failure event and the total volume of associated MTDs are more likely to be more significant under a greenhouse climate, with a relatively smaller amplitude of sea-level changes, than under an icehouse climate.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Carbonate slope failure</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Mass transport deposits</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Tectono-sedimentary evolution</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Controlling factors</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Stratigraphic forward modelling</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Sichuan Basin</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Liu, Keyu</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Salles, Tristan</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Li, Changwei</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">232</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:232</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></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">232</subfield></datafield></record></collection>
score	7.399912

Nicht das Richtige dabei?

Schreiben Sie uns!

Factors controlling carbonate slope failures: Insight from stratigraphic forward modelling

Nicht das Richtige dabei?

Zugang & Verfügbarkeit

Vorhandene Bände

Nicht das Richtige dabei?