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• W4212944265 endingPage "229269" @default.
• W4212944265 startingPage "229269" @default.
• W4212944265 abstract "This study integrates field, geochronological and geochemical data to constrain fluid circulation in the damage and core zone of the seismogenic Monte Morrone Fault System (MMFS), central Apennines (Italy). Faulting along the MMFS evolved from a diffuse deformation at the damage zone towards progressive localisation of a narrower fault core and, finally, to (re)activation of discrete slip surfaces at shallower crustal conditions. Multiple generations of carbonate mineralisations, including veins and slickfibers, occur along the main fault surfaces. Carbonate mineralisations are locally fractured and incorporated in the surrounding cataclasites, documenting repetitive structurally-controlled fluid infiltration during transient episodes of permeability creation and destruction. Stable carbon and oxygen isotopes of the carbonate mineralisations document a dominant meteoric water source probably mixed with deeper circulating waters having longer residence time. Clumped-isotope yield formation temperatures of vein and slickenfibers in the range between 23 and 40 °C. U-Th dating of carbonate mineralisations yield Middle Pleistocene ages (from 268 to 189 ka BP), with a 10–15-ka cyclicity that we link to the coseismic rejuvenation of the structural permeability in the fault zone. We propose that fault-related mineralisations recorded the interactions among tectonic deformation and climate during the Quaternary. Our study is the first documentation of fault-controlled recurrence intervals in fluid infiltration in a seismically active fault of central Apennines. • Fault-related mineralisations record multiple fluid infiltration events. • 10–15 ka cyclicity of fluid ingress is linked with coseismic deformation. • Dated Quaternary syn -tectonic mineralisations are sensitive to climate variations. • Syn-tectonic mineralisations provide an archive for seismic recurrence model." @default.
• W4212944265 created "2022-02-24" @default.
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• W4212944265 date "2022-03-01" @default.
• W4212944265 modified "2023-10-17" @default.
• W4212944265 title "Middle Pleistocene fluid infiltration with 10–15 ka recurrence within the seismic cycle of the active Monte Morrone Fault System (central Apennines, Italy)" @default.
• W4212944265 cites W1511524149 @default.
• W4212944265 cites W1571687464 @default.
• W4212944265 cites W1637801267 @default.
• W4212944265 cites W1674066078 @default.
• W4212944265 cites W1751391025 @default.
• W4212944265 cites W179100328 @default.
• W4212944265 cites W1963680294 @default.
• W4212944265 cites W1965858395 @default.
• W4212944265 cites W1966969423 @default.
• W4212944265 cites W1967107641 @default.
• W4212944265 cites W1968868900 @default.
• W4212944265 cites W1972104383 @default.
• W4212944265 cites W1975769912 @default.
• W4212944265 cites W1979699219 @default.
• W4212944265 cites W1982458478 @default.
• W4212944265 cites W1989006538 @default.
• W4212944265 cites W1995126499 @default.
• W4212944265 cites W2010236289 @default.
• W4212944265 cites W2014133462 @default.
• W4212944265 cites W2017913935 @default.
• W4212944265 cites W2020975371 @default.
• W4212944265 cites W2025520885 @default.
• W4212944265 cites W2026976482 @default.
• W4212944265 cites W2031082350 @default.
• W4212944265 cites W2035843319 @default.
• W4212944265 cites W2040697366 @default.
• W4212944265 cites W2041272962 @default.
• W4212944265 cites W2042400590 @default.
• W4212944265 cites W2047475761 @default.
• W4212944265 cites W2047687600 @default.
• W4212944265 cites W2050972804 @default.
• W4212944265 cites W2052549357 @default.
• W4212944265 cites W2057995713 @default.
• W4212944265 cites W2058259645 @default.
• W4212944265 cites W2059623638 @default.
• W4212944265 cites W2066529194 @default.
• W4212944265 cites W2066555433 @default.
• W4212944265 cites W2074784236 @default.
• W4212944265 cites W2079943478 @default.
• W4212944265 cites W2084129237 @default.
• W4212944265 cites W2084965610 @default.
• W4212944265 cites W2086422338 @default.
• W4212944265 cites W2091751858 @default.
• W4212944265 cites W2092638868 @default.
• W4212944265 cites W2092650977 @default.
• W4212944265 cites W2097944582 @default.
• W4212944265 cites W2101763605 @default.
• W4212944265 cites W2102934491 @default.
• W4212944265 cites W2110527274 @default.
• W4212944265 cites W2112012206 @default.
• W4212944265 cites W2115481049 @default.
• W4212944265 cites W2115563306 @default.
• W4212944265 cites W2115575384 @default.
• W4212944265 cites W2120111675 @default.
• W4212944265 cites W2125952566 @default.
• W4212944265 cites W2127888210 @default.
• W4212944265 cites W2134274598 @default.
• W4212944265 cites W2138776947 @default.
• W4212944265 cites W2144222955 @default.
• W4212944265 cites W2155128667 @default.
• W4212944265 cites W2157020921 @default.
• W4212944265 cites W2157681159 @default.
• W4212944265 cites W2158100493 @default.
• W4212944265 cites W2160400194 @default.
• W4212944265 cites W2161923594 @default.
• W4212944265 cites W2163475804 @default.
• W4212944265 cites W2173255646 @default.
• W4212944265 cites W2267953691 @default.
• W4212944265 cites W2314294150 @default.
• W4212944265 cites W2315789064 @default.
• W4212944265 cites W2323218972 @default.
• W4212944265 cites W2326529832 @default.
• W4212944265 cites W2338437363 @default.
• W4212944265 cites W2404482814 @default.
• W4212944265 cites W2467152113 @default.
• W4212944265 cites W2517123774 @default.
• W4212944265 cites W2518194862 @default.
• W4212944265 cites W2555248423 @default.
• W4212944265 cites W2589919661 @default.
• W4212944265 cites W2603442705 @default.
• W4212944265 cites W2604220874 @default.
• W4212944265 cites W2735617995 @default.
• W4212944265 cites W2750710632 @default.

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