Geology map of Talysh zone: 1 -Holocene (contemporary deposits), 2 -Upper Pleistocene and Holocene, 3 -Pleistocene, inseparated, 4 -Eopleistocene and Lower Pleistocene, 5 -Eopleistocene, 6 -Carboniferous System, 7 -Upper Pliocene, 8 -Upper Miocene and Lower Pliocene, 9 -Upper Miocene, 10 -Middle and Upper Miocene, 11 -Middle Miocene, 12 -Upper Paleocene -Miocene, 13 -Upper Paleocene -Lower Miocene, 14 -Oligocene and Lower Miocene, 15 -Middle and Upper Eocene, 16 -Paleocene and Lower Eocene, 17 -upper part of Middle Jurassic (Callovian) and Upper Jurassic, 18 -Paleogene, 19 -Holocene (adjacent water area of the Caspian Sea: a -authentic, b -supposed).

Geology map of Talysh zone: 1 -Holocene (contemporary deposits), 2 -Upper Pleistocene and Holocene, 3 -Pleistocene, inseparated, 4 -Eopleistocene and Lower Pleistocene, 5 -Eopleistocene, 6 -Carboniferous System, 7 -Upper Pliocene, 8 -Upper Miocene and Lower Pliocene, 9 -Upper Miocene, 10 -Middle and Upper Miocene, 11 -Middle Miocene, 12 -Upper Paleocene -Miocene, 13 -Upper Paleocene -Lower Miocene, 14 -Oligocene and Lower Miocene, 15 -Middle and Upper Eocene, 16 -Paleocene and Lower Eocene, 17 -upper part of Middle Jurassic (Callovian) and Upper Jurassic, 18 -Paleogene, 19 -Holocene (adjacent water area of the Caspian Sea: a -authentic, b -supposed).

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In this paper, we simulate ground motion shaking of the Talysh zone based on the hybrid stochastic-deterministic approach using catalogue-based spatiotemporal analysis for 1970—2019 from the various local and international sources and the fault source pattern. Data for a homogenous and reliable catalogue are obtained from the International Seismolo...

Context in source publication

Context 1
... of porphyritic trachyandesite-basalts and leucite trachyandesites (Peshtasar suite -900-1000 m), which change above to tuffs, tuff-sandstone, tuff-siltstones and shales (Arkivan suite -up to 1000 m) in the Lerik-Yardymly and Buravar zones, while Masally and western part of Lankaranare characterizing with Holocene (contemporary) deposits (Fig. 4) [Azizbekov et al., ...

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