FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2295847358> ?p ?o ?g. }

• W2295847358 abstract "Olkiluoto Island is situated in the northern Baltic Sea, near the southwestern coast of Finland, and is the proposed location of a spent nuclear fuel repository. This study examined Holocene palaeoseismicity in the Olkiluoto area and in the surrounding sea areas by computer simulations together with acousticseismic, sedimentological and dating methods. The most abundant rock type on the island is migmatic mica gneiss, intruded by tonalites, granodiorites and granites. The surrounding Baltic Sea seabed consists of Palaeoproterozoic crystalline bedrock, which is to a great extent covered by younger Mesoproterozoic sedimentary rocks. The area contains several ancient deep-seated fracture zones that divide it into bedrock blocks. The response of bedrock at the Olkiluoto site was modelled considering four future ice-age scenarios. Each scenario produced shear displacements of fractures with different times of occurrence and varying recovery rates. Generally, the larger the maximum ice load, the larger were the permanent shear displacements. For a basic case, the maximum shear displacements were a few centimetres at the proposed nuclear waste repository level, at proximately 500 m b.s.l. High-resolution, low-frequency echo-sounding was used to examine the Holocene submarine sedimentary structures and possible direct and indirect indicators of palaeoseismic activity in the northern Baltic Sea. Echo-sounding profiles of Holocene submarine sediments revealed slides and slumps, normal faults, debris flows and turbidite-type structures. The profiles also showed pockmarks and other structures related to gas or groundwater seepages, which might be related to fracture zone activation. Evidence of postglacial reactivation in the study area was derived from the spatial occurrence of some of the structures, especial the faults and the seepages, in the vicinity of some old bedrock fracture zones." @default.
• W2295847358 created "2016-06-24" @default.
• W2295847358 creator A5078752527 @default.
• W2295847358 date "2007-06-14" @default.
• W2295847358 modified "2023-10-02" @default.
• W2295847358 title "An approach to palaeoseismicity in the Olkiluoto (sea) area during the early Holocene" @default.
• W2295847358 cites W1007428339 @default.
• W2295847358 cites W1535157802 @default.
• W2295847358 cites W1538549717 @default.
• W2295847358 cites W1552623717 @default.
• W2295847358 cites W1558464430 @default.
• W2295847358 cites W1718519193 @default.
• W2295847358 cites W1767087 @default.
• W2295847358 cites W1964944501 @default.
• W2295847358 cites W1965620801 @default.
• W2295847358 cites W1974326113 @default.
• W2295847358 cites W1975635183 @default.
• W2295847358 cites W1976524299 @default.
• W2295847358 cites W1976693889 @default.
• W2295847358 cites W1976724914 @default.
• W2295847358 cites W1976855049 @default.
• W2295847358 cites W1982658490 @default.
• W2295847358 cites W1985720698 @default.
• W2295847358 cites W1987613981 @default.
• W2295847358 cites W1990314669 @default.
• W2295847358 cites W1991185972 @default.
• W2295847358 cites W2001119493 @default.
• W2295847358 cites W2005527884 @default.
• W2295847358 cites W2007236921 @default.
• W2295847358 cites W2012193261 @default.
• W2295847358 cites W2012604835 @default.
• W2295847358 cites W2016195720 @default.
• W2295847358 cites W201829814 @default.
• W2295847358 cites W2020196047 @default.
• W2295847358 cites W2023899869 @default.
• W2295847358 cites W2031333842 @default.
• W2295847358 cites W2031600571 @default.
• W2295847358 cites W2033452743 @default.
• W2295847358 cites W2041046494 @default.
• W2295847358 cites W2042623599 @default.
• W2295847358 cites W2046385652 @default.
• W2295847358 cites W2047413886 @default.
• W2295847358 cites W2051337209 @default.
• W2295847358 cites W2053477507 @default.
• W2295847358 cites W2054408952 @default.
• W2295847358 cites W2055987244 @default.
• W2295847358 cites W2056463665 @default.
• W2295847358 cites W2056743358 @default.
• W2295847358 cites W2058693667 @default.
• W2295847358 cites W2061697657 @default.
• W2295847358 cites W2063608360 @default.
• W2295847358 cites W2076293794 @default.
• W2295847358 cites W2081089014 @default.
• W2295847358 cites W2084832818 @default.
• W2295847358 cites W2089441856 @default.
• W2295847358 cites W2090906201 @default.
• W2295847358 cites W2092486375 @default.
• W2295847358 cites W2093244950 @default.
• W2295847358 cites W2095538800 @default.
• W2295847358 cites W2098126983 @default.
• W2295847358 cites W2103550765 @default.
• W2295847358 cites W2106366209 @default.
• W2295847358 cites W2108463015 @default.
• W2295847358 cites W2112895802 @default.
• W2295847358 cites W2122267972 @default.
• W2295847358 cites W2125111640 @default.
• W2295847358 cites W2131572855 @default.
• W2295847358 cites W2136016125 @default.
• W2295847358 cites W2141006015 @default.
• W2295847358 cites W2146715898 @default.
• W2295847358 cites W2147663465 @default.
• W2295847358 cites W2151038161 @default.
• W2295847358 cites W2167581961 @default.
• W2295847358 cites W2168176303 @default.
• W2295847358 cites W2182912862 @default.
• W2295847358 cites W2184615405 @default.
• W2295847358 cites W2503018929 @default.
• W2295847358 cites W2504148978 @default.
• W2295847358 cites W2742238682 @default.
• W2295847358 cites W2749441542 @default.
• W2295847358 cites W2750555017 @default.
• W2295847358 cites W2910991066 @default.
• W2295847358 cites W3017615021 @default.
• W2295847358 cites W311864639 @default.
• W2295847358 cites W320525870 @default.
• W2295847358 cites W3210986236 @default.
• W2295847358 cites W366803720 @default.
• W2295847358 cites W387249027 @default.
• W2295847358 cites W43623721 @default.
• W2295847358 cites W568979260 @default.
• W2295847358 cites W591431034 @default.
• W2295847358 cites W596716428 @default.
• W2295847358 cites W600586755 @default.
• W2295847358 cites W601790301 @default.
• W2295847358 cites W2186580040 @default.
• W2295847358 cites W2188514370 @default.
• W2295847358 cites W2334982799 @default.
• W2295847358 cites W2499312020 @default.
• W2295847358 hasPublicationYear "2007" @default.
• W2295847358 type Work @default.

• next