FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3138151507> ?p ?o ?g. }

• W3138151507 endingPage "312" @default.
• W3138151507 startingPage "275" @default.
• W3138151507 abstract "Clastic wedges deposited in deep-marine turbidite systems along the circum-Mediterranean region represent key tectonic elements that record the structural growing of the Apennine orogenic belt over the Adria margin. One of these clastic wedges is represented by the Agnone Flysch turbidite succession deposited in the Lagonegro-Molise foredeep basin in the early Messinian, for which the depositional facies and the related processes, as well as the sandstone and mudstone composition are poorly known. A combined sedimentology and sedimentary petrology study has been conducted on this turbidite succession that provides new insight to define the basin architecture and the provenance of the Agnone Flysch during late Miocene. Facies analysis suggests that this turbidite succession is constituted by depositional lobes that were emplaced in a sector of the basin showing a variable morphological confinement with frontal and lateral slope on which turbidite deposits onlapped. Consequently, this topographic context controlled the lateral and vertical distribution of turbidite facies, which record the effects of erosive processes, as well as impact, rebound and reflection processes, in turn related to the flow deceleration induced by structurally-controlled basin confinement. Detailed sandstones compositional analysis indicates a complex unroofing history that reflects structural changes in the source rock units and depositional basin physiography. By combining the sandstone composition with information deduced from the X-ray diffraction (XRD) patterns after thermo-chemical treatments (heating and ethylene glycol treatments), it was possible to explain and predict the sedimentary evolution and geological processes affecting fine grained sediments and, thus, the relationship developed between source area and sedimentary basin. In particular, clay minerals data show that Agnone Flysch experienced an early diagenetic condition as showed by the occurrence of the I/S R0 and I/S R1 on the XRD pattern of the glycolated specimens. The sandstone composition (mainly quartzofeldspathic) shows an increase in the metamorphic rock fragments and a decrease of sedimentary lithics up-section. This compositional trend records, together with the paleocurrents data, a derivation of this material from a mountain range located in the Tyrrhenian sector and from the Calabrian arc terranes." @default.
• W3138151507 created "2021-03-29" @default.
• W3138151507 creator A5006557047 @default.
• W3138151507 creator A5008140750 @default.
• W3138151507 creator A5008220194 @default.
• W3138151507 creator A5016156731 @default.
• W3138151507 creator A5047787603 @default.
• W3138151507 creator A5064928488 @default.
• W3138151507 creator A5080020221 @default.
• W3138151507 creator A5090718497 @default.
• W3138151507 date "2021-06-01" @default.
• W3138151507 modified "2023-09-26" @default.
• W3138151507 title "Facies, composition and provenance of the Agnone Flysch in the context of the early Messinian evolution of the southern Apennine foredeep (Molise, Italy)" @default.
• W3138151507 cites W134906861 @default.
• W3138151507 cites W1485486279 @default.
• W3138151507 cites W1498660521 @default.
• W3138151507 cites W1512437395 @default.
• W3138151507 cites W1527721266 @default.
• W3138151507 cites W1528850606 @default.
• W3138151507 cites W1534110484 @default.
• W3138151507 cites W1570489493 @default.
• W3138151507 cites W1624806571 @default.
• W3138151507 cites W1881051965 @default.
• W3138151507 cites W1907935558 @default.
• W3138151507 cites W1941753701 @default.
• W3138151507 cites W1962066757 @default.
• W3138151507 cites W1963711347 @default.
• W3138151507 cites W1965788398 @default.
• W3138151507 cites W1966066832 @default.
• W3138151507 cites W1966273236 @default.
• W3138151507 cites W1968789454 @default.
• W3138151507 cites W1968964243 @default.
• W3138151507 cites W1970940931 @default.
• W3138151507 cites W1971441077 @default.
• W3138151507 cites W1972280986 @default.
• W3138151507 cites W1972441576 @default.
• W3138151507 cites W1972481325 @default.
• W3138151507 cites W1972996411 @default.
• W3138151507 cites W1973947784 @default.
• W3138151507 cites W1974032102 @default.
• W3138151507 cites W1974558784 @default.
• W3138151507 cites W1977385910 @default.
• W3138151507 cites W1977880023 @default.
• W3138151507 cites W1978758090 @default.
• W3138151507 cites W1983679568 @default.
• W3138151507 cites W1989050618 @default.
• W3138151507 cites W1996657261 @default.
• W3138151507 cites W1999257004 @default.
• W3138151507 cites W2001800904 @default.
• W3138151507 cites W2018999844 @default.
• W3138151507 cites W2021410296 @default.
• W3138151507 cites W2026886308 @default.
• W3138151507 cites W2031052370 @default.
• W3138151507 cites W2035341192 @default.
• W3138151507 cites W2043449144 @default.
• W3138151507 cites W2044247406 @default.
• W3138151507 cites W2045203536 @default.
• W3138151507 cites W2051598312 @default.
• W3138151507 cites W2059358608 @default.
• W3138151507 cites W2063458652 @default.
• W3138151507 cites W2069724073 @default.
• W3138151507 cites W2069987626 @default.
• W3138151507 cites W2070776079 @default.
• W3138151507 cites W2071281979 @default.
• W3138151507 cites W2071715930 @default.
• W3138151507 cites W2073485682 @default.
• W3138151507 cites W2076596567 @default.
• W3138151507 cites W2078063115 @default.
• W3138151507 cites W2079867508 @default.
• W3138151507 cites W2089295860 @default.
• W3138151507 cites W2089645339 @default.
• W3138151507 cites W2091795750 @default.
• W3138151507 cites W2092273609 @default.
• W3138151507 cites W2095442334 @default.
• W3138151507 cites W2098699183 @default.
• W3138151507 cites W2100253244 @default.
• W3138151507 cites W2101874561 @default.
• W3138151507 cites W2108540145 @default.
• W3138151507 cites W2109934455 @default.
• W3138151507 cites W2115471531 @default.
• W3138151507 cites W2115563306 @default.
• W3138151507 cites W2117814431 @default.
• W3138151507 cites W2118755672 @default.
• W3138151507 cites W2120935731 @default.
• W3138151507 cites W2127251611 @default.
• W3138151507 cites W2127372790 @default.
• W3138151507 cites W2128776046 @default.
• W3138151507 cites W2129194942 @default.
• W3138151507 cites W2130579245 @default.
• W3138151507 cites W2132223903 @default.
• W3138151507 cites W2133343279 @default.
• W3138151507 cites W2134308193 @default.
• W3138151507 cites W2135008648 @default.
• W3138151507 cites W2136524557 @default.
• W3138151507 cites W2141235941 @default.
• W3138151507 cites W2142148850 @default.
• W3138151507 cites W2147432383 @default.
• W3138151507 cites W2150826815 @default.

• next