Response of sedimentary and pollen records to the 1933 Diexi earthquake on the eastern Tibetan Plateau

Vegetation plays an important role in ecosystem stability in tectonically active regions such as the eastern Tibetan Plateau (ETP). To determine the response of mountain ecosystem to climate change and tectonic activity on the ETP, detailed analyses of chronology, pollen, grain size and magnetic sus...
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Autor*in:	Xiaotong Wei [verfasserIn] Hanchao Jiang [verfasserIn] Hongyan Xu [verfasserIn] Jiawei Fan [verfasserIn] Wei Shi [verfasserIn] Qiaoqiao Guo [verfasserIn] Siqi Zhang [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2021

Schlagwörter:	Ecosystem stability Climate change Tectonic activity Diexi earthquake Lacustrine sediments Eastern Tibetan Plateau

Übergeordnetes Werk:	In: Ecological Indicators - Elsevier, 2021, 129(2021), Seite 107887-
Übergeordnetes Werk:	volume:129 ; year:2021 ; pages:107887-

Links:	Link aufrufen Link aufrufen Link aufrufen Journal toc

DOI / URN:	10.1016/j.ecolind.2021.107887

Katalog-ID:	DOAJ077554256

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650		4	\|a Ecosystem stability
650		4	\|a Climate change
650		4	\|a Tectonic activity
650		4	\|a Diexi earthquake
650		4	\|a Lacustrine sediments
650		4	\|a Eastern Tibetan Plateau
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700	0		\|a Siqi Zhang \|e verfasserin \|4 aut
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spelling	10.1016/j.ecolind.2021.107887 doi (DE-627)DOAJ077554256 (DE-599)DOAJcf4618331c3d40efa3a25e498ef1a868 DE-627 ger DE-627 rakwb eng QH540-549.5 Xiaotong Wei verfasserin aut Response of sedimentary and pollen records to the 1933 Diexi earthquake on the eastern Tibetan Plateau 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Vegetation plays an important role in ecosystem stability in tectonically active regions such as the eastern Tibetan Plateau (ETP). To determine the response of mountain ecosystem to climate change and tectonic activity on the ETP, detailed analyses of chronology, pollen, grain size and magnetic susceptibility (SUS) were conducted on a lacustrine sequence from the upper reaches of the Min River. The results show that the lacustrine sediments are mainly transported by wind as those seismogenic dust at Diexi and Lixian. The fine–grained sediments (<20 μm) are background dust that was transported over a long distance, while the coarse-grained sediments (<20 μm) were transported from local to regional dust sources. Intriguingly, the sand fraction (<63 μm) suddenly increased by 10.4%, in response to the Diexi Ms 7.5 earthquake in 1933. The earthquake probably induced many large landslides and provided more sources of coarse particles close to the study area. Also, around 1933, coniferous pollen increased rapidly while herbaceous and aquatic plants decreased significantly, probably due to a marked change in the local hydrological conditions caused by the strong earthquake. The percentage of shrub pollen dominated by Hippophae, remained at a relatively high level, showing these plants to have great significance for ecological stability in tectonically active regions. Ecosystem stability Climate change Tectonic activity Diexi earthquake Lacustrine sediments Eastern Tibetan Plateau Ecology Hanchao Jiang verfasserin aut Hongyan Xu verfasserin aut Jiawei Fan verfasserin aut Wei Shi verfasserin aut Qiaoqiao Guo verfasserin aut Siqi Zhang verfasserin aut In Ecological Indicators Elsevier, 2021 129(2021), Seite 107887- (DE-627)338074163 (DE-600)2063587-4 18727034 nnns volume:129 year:2021 pages:107887- https://doi.org/10.1016/j.ecolind.2021.107887 kostenfrei https://doaj.org/article/cf4618331c3d40efa3a25e498ef1a868 kostenfrei http://www.sciencedirect.com/science/article/pii/S1470160X21005525 kostenfrei https://doaj.org/toc/1470-160X Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 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_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_602 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2008 GBV_ILN_2014 GBV_ILN_2025 GBV_ILN_2034 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2064 GBV_ILN_2106 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2122 GBV_ILN_2143 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 129 2021 107887-
allfields_unstemmed	10.1016/j.ecolind.2021.107887 doi (DE-627)DOAJ077554256 (DE-599)DOAJcf4618331c3d40efa3a25e498ef1a868 DE-627 ger DE-627 rakwb eng QH540-549.5 Xiaotong Wei verfasserin aut Response of sedimentary and pollen records to the 1933 Diexi earthquake on the eastern Tibetan Plateau 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Vegetation plays an important role in ecosystem stability in tectonically active regions such as the eastern Tibetan Plateau (ETP). To determine the response of mountain ecosystem to climate change and tectonic activity on the ETP, detailed analyses of chronology, pollen, grain size and magnetic susceptibility (SUS) were conducted on a lacustrine sequence from the upper reaches of the Min River. The results show that the lacustrine sediments are mainly transported by wind as those seismogenic dust at Diexi and Lixian. The fine–grained sediments (<20 μm) are background dust that was transported over a long distance, while the coarse-grained sediments (<20 μm) were transported from local to regional dust sources. Intriguingly, the sand fraction (<63 μm) suddenly increased by 10.4%, in response to the Diexi Ms 7.5 earthquake in 1933. The earthquake probably induced many large landslides and provided more sources of coarse particles close to the study area. Also, around 1933, coniferous pollen increased rapidly while herbaceous and aquatic plants decreased significantly, probably due to a marked change in the local hydrological conditions caused by the strong earthquake. The percentage of shrub pollen dominated by Hippophae, remained at a relatively high level, showing these plants to have great significance for ecological stability in tectonically active regions. Ecosystem stability Climate change Tectonic activity Diexi earthquake Lacustrine sediments Eastern Tibetan Plateau Ecology Hanchao Jiang verfasserin aut Hongyan Xu verfasserin aut Jiawei Fan verfasserin aut Wei Shi verfasserin aut Qiaoqiao Guo verfasserin aut Siqi Zhang verfasserin aut In Ecological Indicators Elsevier, 2021 129(2021), Seite 107887- (DE-627)338074163 (DE-600)2063587-4 18727034 nnns volume:129 year:2021 pages:107887- https://doi.org/10.1016/j.ecolind.2021.107887 kostenfrei https://doaj.org/article/cf4618331c3d40efa3a25e498ef1a868 kostenfrei http://www.sciencedirect.com/science/article/pii/S1470160X21005525 kostenfrei https://doaj.org/toc/1470-160X Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 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_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_602 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2008 GBV_ILN_2014 GBV_ILN_2025 GBV_ILN_2034 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2064 GBV_ILN_2106 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2122 GBV_ILN_2143 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 129 2021 107887-
allfieldsGer	10.1016/j.ecolind.2021.107887 doi (DE-627)DOAJ077554256 (DE-599)DOAJcf4618331c3d40efa3a25e498ef1a868 DE-627 ger DE-627 rakwb eng QH540-549.5 Xiaotong Wei verfasserin aut Response of sedimentary and pollen records to the 1933 Diexi earthquake on the eastern Tibetan Plateau 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Vegetation plays an important role in ecosystem stability in tectonically active regions such as the eastern Tibetan Plateau (ETP). To determine the response of mountain ecosystem to climate change and tectonic activity on the ETP, detailed analyses of chronology, pollen, grain size and magnetic susceptibility (SUS) were conducted on a lacustrine sequence from the upper reaches of the Min River. The results show that the lacustrine sediments are mainly transported by wind as those seismogenic dust at Diexi and Lixian. The fine–grained sediments (<20 μm) are background dust that was transported over a long distance, while the coarse-grained sediments (<20 μm) were transported from local to regional dust sources. Intriguingly, the sand fraction (<63 μm) suddenly increased by 10.4%, in response to the Diexi Ms 7.5 earthquake in 1933. The earthquake probably induced many large landslides and provided more sources of coarse particles close to the study area. Also, around 1933, coniferous pollen increased rapidly while herbaceous and aquatic plants decreased significantly, probably due to a marked change in the local hydrological conditions caused by the strong earthquake. The percentage of shrub pollen dominated by Hippophae, remained at a relatively high level, showing these plants to have great significance for ecological stability in tectonically active regions. Ecosystem stability Climate change Tectonic activity Diexi earthquake Lacustrine sediments Eastern Tibetan Plateau Ecology Hanchao Jiang verfasserin aut Hongyan Xu verfasserin aut Jiawei Fan verfasserin aut Wei Shi verfasserin aut Qiaoqiao Guo verfasserin aut Siqi Zhang verfasserin aut In Ecological Indicators Elsevier, 2021 129(2021), Seite 107887- (DE-627)338074163 (DE-600)2063587-4 18727034 nnns volume:129 year:2021 pages:107887- https://doi.org/10.1016/j.ecolind.2021.107887 kostenfrei https://doaj.org/article/cf4618331c3d40efa3a25e498ef1a868 kostenfrei http://www.sciencedirect.com/science/article/pii/S1470160X21005525 kostenfrei https://doaj.org/toc/1470-160X Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 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_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_602 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2008 GBV_ILN_2014 GBV_ILN_2025 GBV_ILN_2034 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2064 GBV_ILN_2106 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2122 GBV_ILN_2143 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 129 2021 107887-
allfieldsSound	10.1016/j.ecolind.2021.107887 doi (DE-627)DOAJ077554256 (DE-599)DOAJcf4618331c3d40efa3a25e498ef1a868 DE-627 ger DE-627 rakwb eng QH540-549.5 Xiaotong Wei verfasserin aut Response of sedimentary and pollen records to the 1933 Diexi earthquake on the eastern Tibetan Plateau 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Vegetation plays an important role in ecosystem stability in tectonically active regions such as the eastern Tibetan Plateau (ETP). To determine the response of mountain ecosystem to climate change and tectonic activity on the ETP, detailed analyses of chronology, pollen, grain size and magnetic susceptibility (SUS) were conducted on a lacustrine sequence from the upper reaches of the Min River. The results show that the lacustrine sediments are mainly transported by wind as those seismogenic dust at Diexi and Lixian. The fine–grained sediments (<20 μm) are background dust that was transported over a long distance, while the coarse-grained sediments (<20 μm) were transported from local to regional dust sources. Intriguingly, the sand fraction (<63 μm) suddenly increased by 10.4%, in response to the Diexi Ms 7.5 earthquake in 1933. The earthquake probably induced many large landslides and provided more sources of coarse particles close to the study area. Also, around 1933, coniferous pollen increased rapidly while herbaceous and aquatic plants decreased significantly, probably due to a marked change in the local hydrological conditions caused by the strong earthquake. The percentage of shrub pollen dominated by Hippophae, remained at a relatively high level, showing these plants to have great significance for ecological stability in tectonically active regions. Ecosystem stability Climate change Tectonic activity Diexi earthquake Lacustrine sediments Eastern Tibetan Plateau Ecology Hanchao Jiang verfasserin aut Hongyan Xu verfasserin aut Jiawei Fan verfasserin aut Wei Shi verfasserin aut Qiaoqiao Guo verfasserin aut Siqi Zhang verfasserin aut In Ecological Indicators Elsevier, 2021 129(2021), Seite 107887- (DE-627)338074163 (DE-600)2063587-4 18727034 nnns volume:129 year:2021 pages:107887- https://doi.org/10.1016/j.ecolind.2021.107887 kostenfrei https://doaj.org/article/cf4618331c3d40efa3a25e498ef1a868 kostenfrei http://www.sciencedirect.com/science/article/pii/S1470160X21005525 kostenfrei https://doaj.org/toc/1470-160X Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 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_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_602 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2008 GBV_ILN_2014 GBV_ILN_2025 GBV_ILN_2034 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2064 GBV_ILN_2106 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2122 GBV_ILN_2143 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 129 2021 107887-
language	English
source	In Ecological Indicators 129(2021), Seite 107887- volume:129 year:2021 pages:107887-
sourceStr	In Ecological Indicators 129(2021), Seite 107887- volume:129 year:2021 pages:107887-
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	Ecosystem stability Climate change Tectonic activity Diexi earthquake Lacustrine sediments Eastern Tibetan Plateau Ecology
isfreeaccess_bool	true
container_title	Ecological Indicators
authorswithroles_txt_mv	Xiaotong Wei @@aut@@ Hanchao Jiang @@aut@@ Hongyan Xu @@aut@@ Jiawei Fan @@aut@@ Wei Shi @@aut@@ Qiaoqiao Guo @@aut@@ Siqi Zhang @@aut@@
publishDateDaySort_date	2021-01-01T00:00:00Z
hierarchy_top_id	338074163
id	DOAJ077554256
language_de	englisch
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callnumber-first	Q - Science
author	Xiaotong Wei
spellingShingle	Xiaotong Wei misc QH540-549.5 misc Ecosystem stability misc Climate change misc Tectonic activity misc Diexi earthquake misc Lacustrine sediments misc Eastern Tibetan Plateau misc Ecology Response of sedimentary and pollen records to the 1933 Diexi earthquake on the eastern Tibetan Plateau
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topic_title	QH540-549.5 Response of sedimentary and pollen records to the 1933 Diexi earthquake on the eastern Tibetan Plateau Ecosystem stability Climate change Tectonic activity Diexi earthquake Lacustrine sediments Eastern Tibetan Plateau
topic	misc QH540-549.5 misc Ecosystem stability misc Climate change misc Tectonic activity misc Diexi earthquake misc Lacustrine sediments misc Eastern Tibetan Plateau misc Ecology
topic_unstemmed	misc QH540-549.5 misc Ecosystem stability misc Climate change misc Tectonic activity misc Diexi earthquake misc Lacustrine sediments misc Eastern Tibetan Plateau misc Ecology
topic_browse	misc QH540-549.5 misc Ecosystem stability misc Climate change misc Tectonic activity misc Diexi earthquake misc Lacustrine sediments misc Eastern Tibetan Plateau misc Ecology
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title	Response of sedimentary and pollen records to the 1933 Diexi earthquake on the eastern Tibetan Plateau
ctrlnum	(DE-627)DOAJ077554256 (DE-599)DOAJcf4618331c3d40efa3a25e498ef1a868
title_full	Response of sedimentary and pollen records to the 1933 Diexi earthquake on the eastern Tibetan Plateau
author_sort	Xiaotong Wei
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author_browse	Xiaotong Wei Hanchao Jiang Hongyan Xu Jiawei Fan Wei Shi Qiaoqiao Guo Siqi Zhang
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title_sort	response of sedimentary and pollen records to the 1933 diexi earthquake on the eastern tibetan plateau
callnumber	QH540-549.5
title_auth	Response of sedimentary and pollen records to the 1933 Diexi earthquake on the eastern Tibetan Plateau
abstract	Vegetation plays an important role in ecosystem stability in tectonically active regions such as the eastern Tibetan Plateau (ETP). To determine the response of mountain ecosystem to climate change and tectonic activity on the ETP, detailed analyses of chronology, pollen, grain size and magnetic susceptibility (SUS) were conducted on a lacustrine sequence from the upper reaches of the Min River. The results show that the lacustrine sediments are mainly transported by wind as those seismogenic dust at Diexi and Lixian. The fine–grained sediments (<20 μm) are background dust that was transported over a long distance, while the coarse-grained sediments (<20 μm) were transported from local to regional dust sources. Intriguingly, the sand fraction (<63 μm) suddenly increased by 10.4%, in response to the Diexi Ms 7.5 earthquake in 1933. The earthquake probably induced many large landslides and provided more sources of coarse particles close to the study area. Also, around 1933, coniferous pollen increased rapidly while herbaceous and aquatic plants decreased significantly, probably due to a marked change in the local hydrological conditions caused by the strong earthquake. The percentage of shrub pollen dominated by Hippophae, remained at a relatively high level, showing these plants to have great significance for ecological stability in tectonically active regions.
abstractGer	Vegetation plays an important role in ecosystem stability in tectonically active regions such as the eastern Tibetan Plateau (ETP). To determine the response of mountain ecosystem to climate change and tectonic activity on the ETP, detailed analyses of chronology, pollen, grain size and magnetic susceptibility (SUS) were conducted on a lacustrine sequence from the upper reaches of the Min River. The results show that the lacustrine sediments are mainly transported by wind as those seismogenic dust at Diexi and Lixian. The fine–grained sediments (<20 μm) are background dust that was transported over a long distance, while the coarse-grained sediments (<20 μm) were transported from local to regional dust sources. Intriguingly, the sand fraction (<63 μm) suddenly increased by 10.4%, in response to the Diexi Ms 7.5 earthquake in 1933. The earthquake probably induced many large landslides and provided more sources of coarse particles close to the study area. Also, around 1933, coniferous pollen increased rapidly while herbaceous and aquatic plants decreased significantly, probably due to a marked change in the local hydrological conditions caused by the strong earthquake. The percentage of shrub pollen dominated by Hippophae, remained at a relatively high level, showing these plants to have great significance for ecological stability in tectonically active regions.
abstract_unstemmed	Vegetation plays an important role in ecosystem stability in tectonically active regions such as the eastern Tibetan Plateau (ETP). To determine the response of mountain ecosystem to climate change and tectonic activity on the ETP, detailed analyses of chronology, pollen, grain size and magnetic susceptibility (SUS) were conducted on a lacustrine sequence from the upper reaches of the Min River. The results show that the lacustrine sediments are mainly transported by wind as those seismogenic dust at Diexi and Lixian. The fine–grained sediments (<20 μm) are background dust that was transported over a long distance, while the coarse-grained sediments (<20 μm) were transported from local to regional dust sources. Intriguingly, the sand fraction (<63 μm) suddenly increased by 10.4%, in response to the Diexi Ms 7.5 earthquake in 1933. The earthquake probably induced many large landslides and provided more sources of coarse particles close to the study area. Also, around 1933, coniferous pollen increased rapidly while herbaceous and aquatic plants decreased significantly, probably due to a marked change in the local hydrological conditions caused by the strong earthquake. The percentage of shrub pollen dominated by Hippophae, remained at a relatively high level, showing these plants to have great significance for ecological stability in tectonically active regions.
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title_short	Response of sedimentary and pollen records to the 1933 Diexi earthquake on the eastern Tibetan Plateau
url	https://doi.org/10.1016/j.ecolind.2021.107887 https://doaj.org/article/cf4618331c3d40efa3a25e498ef1a868 http://www.sciencedirect.com/science/article/pii/S1470160X21005525 https://doaj.org/toc/1470-160X
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score	7.400256

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Response of sedimentary and pollen records to the 1933 Diexi earthquake on the eastern Tibetan Plateau

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Zugang & Verfügbarkeit

Vorhandene Bände

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