About: Seismic hazard in the Marmara Sea region following the 17 August 1999 Izmit earthquake

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scientific article published in Nature

Attributes	Values
rdf:type	Item
description	artículu científicu (ast) wetenschappelijk artikel (nl) wüsseschaftlicher Artikel, wo im März 2000 veröffentlicht worden isch (gsw) im März 2000 veröffentlichter wissenschaftlicher Artikel (de) article publié dans la revue scientifique Nature (fr) নেচারে প্রকাশিত বৈজ্ঞানিক প্রবন্ধ (bn) scientific article published in Nature (en) Նեյչրում հրատարակված հոդված (hy) наукова стаття, опублікована в Nature в березні 2000 (uk)
publication date	wds:Q57128877-EBFEE2D8-9DC7-4160-BC4A-4A17D3B8A7C5
publication date	2000-03-01 00:00:00Z (xsd:dateTime)
language of work or name	wds:Q57128877-5D0876C2-B225-4702-8CB2-837AD4D18D74
language of work or name	English
exact match	wds:Q57128877-0A20FD04-F7E4-4273-BECB-5A252FBCCFE6
exact match	https://scigraph.springernature.com/pub.10.1038/35005054
cites work	wds:Q57128877-03C53272-93C6-4BB6-A9B2-8306DB89D372 wds:Q57128877-0E75B29F-1C89-40AF-BCFB-E4F502BD0C4E wds:Q57128877-2C7CB676-A827-4B0F-AAA3-4A79213A77B2 wds:Q57128877-546EB87B-42CC-4778-8E5D-82FA05E48013 wds:Q57128877-606EC010-79FC-42D7-9AC5-0FC791236B96 wds:Q57128877-70FD67EF-3382-47E2-A86F-4C1AD3B72C96 wds:Q57128877-77F8DBE7-7832-40BD-8AC0-EB781712A14C wds:Q57128877-7D2D61F8-EAAD-472D-B8F4-490CAD23337C wds:Q57128877-CC15EA19-9E30-41F2-AB91-1CFE4B6A7AD6 wds:Q57128877-D23D0554-61E8-4E02-BEEA-F4DD68EE522C
cites work	Tomographic evidence for localized lithospheric shear along the altyn tagh fault An observational test of the critical earthquake concept A constitutive law for rate of earthquake production and its application to earthquake clustering Progressive failure on the North Anatolian fault since 1939 by earthquake stress triggering Global Positioning System measurements of present-day crustal movements in the Arabia-Africa-Eurasia plate collision zone GEOLOGY:Enhanced: The 17 August 1999 Izmit Earthquake Slip deficit on the san andreas fault at parkfield, california, as revealed by inversion of geodetic data. In the shadow of 1857-the effect of the Great Ft. Tejon Earthquake on subsequent earthquakes in southern California Westward propagation of the North Anatolian fault into the northern Aegean: Timing and kinematics Introduction to Special Section: Stress Triggers, Stress Shadows, and Implications for Seismic Hazard
author name string	wds:Q57128877-2BC9FBEC-4874-4E5F-976F-7F7E157795A1 wds:Q57128877-399375A0-BACB-4D23-8417-E339E6EB6AEA wds:Q57128877-7F74F0A2-3BF7-48E0-AF94-6C101002FEC5 wds:Q57128877-91D77509-FD1C-473D-85B0-333DD8ECA866 wds:Q57128877-BE81A9EF-3EBB-42C5-BD41-02C411BA9768 wds:Q57128877-F59E68BA-55B2-4A38-934F-5CD4EAC489B0
author name string	Jacques E Meyer B King GC Barka A Hubert-Ferrari A Tapponnier P
rdfs:label	Seismic hazard in the Marmara Sea region following the 17 August 1999 Izmit earthquake (en) Seismic hazard in the Marmara Sea region following the 17 August 1999 Izmit earthquake (nl)
skos:prefLabel	Seismic hazard in the Marmara Sea region following the 17 August 1999 Izmit earthquake (en) Seismic hazard in the Marmara Sea region following the 17 August 1999 Izmit earthquake (nl)
name	Seismic hazard in the Marmara Sea region following the 17 August 1999 Izmit earthquake (en) Seismic hazard in the Marmara Sea region following the 17 August 1999 Izmit earthquake (nl)
author	wds:Q57128877-0CC8123D-719D-4CDA-8306-CB5273978D35 wds:Q57128877-CB34E57C-2F27-447D-A53A-B1D07706B4A8
author	Rolando Armijo Suleyman Sami Nalbant
title	wds:Q57128877-A42FDEB3-7A41-4DD1-8240-9A90EA6555F1
title	Seismic hazard in the Marmara Sea region following the 17 August 1999 Izmit earthquake (en)
page(s)	wds:Q57128877-EA408635-F338-4312-9503-B23B0521A243
page(s)	269-273
instance of	wds:Q57128877-9E0B776F-9631-48DD-A49B-57EDC407187D
instance of	scholarly article
main subject	wds:Q57128877-5E19DADB-8AB7-4B77-BD9E-62FEB3282236 wds:Q57128877-6b5d0237-4b8b-89e7-a0af-54f1be577787
main subject	earthquake 1999 İzmit earthquake
PubMed ID	wds:Q57128877-C7E3DA45-7B7D-4B9F-96F6-FC9B3970BFD2
PubMed ID	http://rdf.ncbi.nlm.nih.gov/pubchem/reference/10749206
PubMed ID	10749206
published in	wds:Q57128877-1C53C04E-274B-43BD-ADAE-CDBA1760E513
published in	Nature
issue	wds:Q57128877-DADA8128-D9FB-42E9-A03A-E0597F24BE66
volume	wds:Q57128877-9D8EAD31-1B58-40DB-8319-F15614245C4D
issue	6775
volume	404
DOI	wds:Q57128877-C9D62FE6-4337-46E5-8CC9-3B341387D71E
DOI	http://dx.doi.org/10.1038/35005054
DOI	10.1038/35005054
Dimensions Publication ID	wds:Q57128877-BF571B49-3B3F-431B-B3A5-5488D96D6C6A
Dimensions Publication ID	1043696841
is about of	https://www.wikidata.org/wiki/Special:EntityData/Q57128877
is cites work of	GPS constraints on continental deformation in the Africa-Arabia-Eurasia continental collision zone and implications for the dynamics of plate interactions M ≥ 7 earthquake rupture forecast and time-dependent probability for the sea of Marmara region, Turkey Recalculated probability of M≥ 7 earthquakes beneath the Sea of Marmara, Turkey Stress changes from the 2008 Wenchuan earthquake and increased hazard in the Sichuan basin Block models of crustal motion in southern California constrained by GPS measurements Significance of stress transfer in time-dependent earthquake probability calculations Interactive editing of digital fault models Asymmetric slip partitioning in the Sea of Marmara pull-apart: a clue to propagation processes of the North Anatolian Fault? An earthquake gap south of Istanbul Submarine fault scarps in the Sea of Marmara pull-apart (North Anatolian Fault): Implications for seismic hazard in Istanbul Hagia Sophia: Shaken, not stirred Indonesian earthquake: earthquake risk from co-seismic stress North Anatolian Fault in the Gulf of Izmit (Turkey): Rapid vertical motion in response to minor bends of a nonvertical continental transform Morphology, displacement, and slip rates along the North Anatolian Fault, Turkey Earthquake crisis unveils the growth of an incipient continental fault system Precursory accelerating seismic crustal deformation in the Northwestern Anatolia Fault Zone Normal fault interaction caused by coseismic and postseismic stress changes

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