Matches in SemOpenAlex for { <https://semopenalex.org/work/W2017022013> ?p ?o ?g. }
- W2017022013 endingPage "872" @default.
- W2017022013 startingPage "854" @default.
- W2017022013 abstract "Detailed multibeam, sedimentological, and geophysical surveys provide ample new data to confirm that the Anaximander Mountains (Eastern Mediterranean) are an important area for active mud volcanism and gas hydrate formation. More than 3000 km of multibeam track length was acquired during two recent missions and 80 gravity and box cores were recovered. Morphology and backscatter data of the study area have better resolution than previous surveys, and very detailed morphology maps have been made of the known targeted mud volcanoes (Amsterdam, Kazan and Kula), especially the Amsterdam “crater” and the related mud breccia flows. Gas hydrates collected repeatedly from a large area of Amsterdam mud volcano at a sub-bottom depth of around 0.3–1.5 m resemble compacted snow and have a rather flaky form. New gas hydrate sites were found at Amsterdam mud volcano, including the mud flow sloping off to the south. Gas hydrates sampled for the first time at Kazan mud volcano are dispersed throughout the core samples deeper than 0.3 m and display a ‘rice’-like appearance. Relative chronology and AMS dating of interbedded pelagic sediments (Late Holocene hemipelagic, sapropel layer S1 and ash layers) within the mud flows indicate that successive eruptions of Kula mud volcano have a periodicity of about 5–10 kyrs. New mud volcanoes identified on the basis of multibeam backscatter intensity were sampled, documented as active and named “Athina” and “Thessaloniki”. Gas hydrates were sampled also in Thessaloniki mud volcano, the shallowest (1264 m) among all the active Mediterranean sites, at the boundary of the gas hydrate stability zone. Biostratigraphical analyses of mud breccia clasts indicated that the source of the subsurface sedimentary sequences consists of Late Cretaceous limestones, Paleocene siliciclastic rocks, Eocene biogenic limestones and Miocene mudstones. Rough estimations of the total capacity of the Anaximander mud volcanoes in methane gas are 2.56–6.40 km3." @default.
- W2017022013 created "2016-06-24" @default.
- W2017022013 creator A5003733001 @default.
- W2017022013 creator A5005282150 @default.
- W2017022013 creator A5008034740 @default.
- W2017022013 creator A5016182605 @default.
- W2017022013 creator A5021690875 @default.
- W2017022013 creator A5024723684 @default.
- W2017022013 creator A5029330138 @default.
- W2017022013 creator A5032468594 @default.
- W2017022013 creator A5042058671 @default.
- W2017022013 creator A5043104749 @default.
- W2017022013 creator A5045232774 @default.
- W2017022013 creator A5073941887 @default.
- W2017022013 creator A5075071181 @default.
- W2017022013 creator A5075475670 @default.
- W2017022013 date "2009-06-01" @default.
- W2017022013 modified "2023-10-18" @default.
- W2017022013 title "Mud volcanoes and gas hydrates in the Anaximander mountains (Eastern Mediterranean Sea)" @default.
- W2017022013 cites W1977858881 @default.
- W2017022013 cites W1991816052 @default.
- W2017022013 cites W1992270346 @default.
- W2017022013 cites W1997468419 @default.
- W2017022013 cites W1998222714 @default.
- W2017022013 cites W1999982208 @default.
- W2017022013 cites W2001830268 @default.
- W2017022013 cites W2011979724 @default.
- W2017022013 cites W2013294597 @default.
- W2017022013 cites W2015289795 @default.
- W2017022013 cites W2015579553 @default.
- W2017022013 cites W2023920049 @default.
- W2017022013 cites W2024961541 @default.
- W2017022013 cites W2033497568 @default.
- W2017022013 cites W2034674035 @default.
- W2017022013 cites W2036040130 @default.
- W2017022013 cites W2036148312 @default.
- W2017022013 cites W2037582666 @default.
- W2017022013 cites W2050679673 @default.
- W2017022013 cites W2064940645 @default.
- W2017022013 cites W2071165731 @default.
- W2017022013 cites W2072741523 @default.
- W2017022013 cites W2088964382 @default.
- W2017022013 cites W2093642490 @default.
- W2017022013 cites W2100045328 @default.
- W2017022013 cites W2101997015 @default.
- W2017022013 cites W2108193635 @default.
- W2017022013 cites W2112019984 @default.
- W2017022013 cites W2125324504 @default.
- W2017022013 cites W2127616548 @default.
- W2017022013 cites W2146283003 @default.
- W2017022013 cites W2151529013 @default.
- W2017022013 cites W2162559981 @default.
- W2017022013 cites W2493918850 @default.
- W2017022013 cites W2552616333 @default.
- W2017022013 cites W4234701869 @default.
- W2017022013 doi "https://doi.org/10.1016/j.marpetgeo.2008.05.002" @default.
- W2017022013 hasPublicationYear "2009" @default.
- W2017022013 type Work @default.
- W2017022013 sameAs 2017022013 @default.
- W2017022013 citedByCount "74" @default.
- W2017022013 countsByYear W20170220132012 @default.
- W2017022013 countsByYear W20170220132013 @default.
- W2017022013 countsByYear W20170220132014 @default.
- W2017022013 countsByYear W20170220132015 @default.
- W2017022013 countsByYear W20170220132016 @default.
- W2017022013 countsByYear W20170220132017 @default.
- W2017022013 countsByYear W20170220132018 @default.
- W2017022013 countsByYear W20170220132019 @default.
- W2017022013 countsByYear W20170220132020 @default.
- W2017022013 countsByYear W20170220132021 @default.
- W2017022013 countsByYear W20170220132022 @default.
- W2017022013 countsByYear W20170220132023 @default.
- W2017022013 crossrefType "journal-article" @default.
- W2017022013 hasAuthorship W2017022013A5003733001 @default.
- W2017022013 hasAuthorship W2017022013A5005282150 @default.
- W2017022013 hasAuthorship W2017022013A5008034740 @default.
- W2017022013 hasAuthorship W2017022013A5016182605 @default.
- W2017022013 hasAuthorship W2017022013A5021690875 @default.
- W2017022013 hasAuthorship W2017022013A5024723684 @default.
- W2017022013 hasAuthorship W2017022013A5029330138 @default.
- W2017022013 hasAuthorship W2017022013A5032468594 @default.
- W2017022013 hasAuthorship W2017022013A5042058671 @default.
- W2017022013 hasAuthorship W2017022013A5043104749 @default.
- W2017022013 hasAuthorship W2017022013A5045232774 @default.
- W2017022013 hasAuthorship W2017022013A5073941887 @default.
- W2017022013 hasAuthorship W2017022013A5075071181 @default.
- W2017022013 hasAuthorship W2017022013A5075475670 @default.
- W2017022013 hasConcept C100402318 @default.
- W2017022013 hasConcept C114793014 @default.
- W2017022013 hasConcept C120806208 @default.
- W2017022013 hasConcept C121332964 @default.
- W2017022013 hasConcept C127313418 @default.
- W2017022013 hasConcept C1276947 @default.
- W2017022013 hasConcept C146348940 @default.
- W2017022013 hasConcept C151730666 @default.
- W2017022013 hasConcept C161509811 @default.
- W2017022013 hasConcept C17409809 @default.
- W2017022013 hasConcept C178790620 @default.