FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2563939710> ?p ?o ?g. }

• W2563939710 endingPage "433" @default.
• W2563939710 startingPage "422" @default.
• W2563939710 abstract "Seismic reflection data and field observations have revealed the presence of voluminous igneous sill complexes emplaced into organic-rich shale formations in sedimentary basins worldwide. Damage and structures associated with sills have major implications for fluid flow through basins. Constraining the distribution of these structures requires a good understanding of the sill emplacement mechanism. However, most mechanical models of sill emplacement assume elastic host behaviour, whereas shale is expected to deform inelastically. This contradiction calls for new field observations to better constrain sill emplacement mechanisms. In this paper, we report on detailed field observations of spectacularly exposed fingers and a sill emplaced in shale at Cuesta del Chihuido, in the Neuquen Basin, Argentina. Exceptional outcrop conditions allow detailed descriptions of both (1) the entire cross-section of the intrusions, and (2) the deformation structures accommodating intrusion propagation in the host rock. All intrusions exhibit irregular, blunt or rectangular tips. The structures accommodating the tip propagation are systematically compressional, including reverse faults, folding and imbricate thrust system. Our observations suggest that the studied intrusions have propagated by pushing the host rock ahead, as a viscous indenter. Our observations suggest that the viscous indenter model is probably a dominant mechanism of sill emplacement in shale." @default.
• W2563939710 created "2017-01-06" @default.
• W2563939710 creator A5012927423 @default.
• W2563939710 creator A5024579406 @default.
• W2563939710 creator A5068105372 @default.
• W2563939710 creator A5075766872 @default.
• W2563939710 date "2016-12-22" @default.
• W2563939710 modified "2023-10-18" @default.
• W2563939710 title "Igneous sill and finger emplacement mechanism in shale-dominated formations: a field study at Cuesta del Chihuido, Neuquén Basin, Argentina" @default.
• W2563939710 cites W1485921491 @default.
• W2563939710 cites W1551370108 @default.
• W2563939710 cites W1562549681 @default.
• W2563939710 cites W1922701939 @default.
• W2563939710 cites W1965125081 @default.
• W2563939710 cites W1973774692 @default.
• W2563939710 cites W1974536910 @default.
• W2563939710 cites W1974975954 @default.
• W2563939710 cites W1975819325 @default.
• W2563939710 cites W1977259495 @default.
• W2563939710 cites W1984305821 @default.
• W2563939710 cites W1986617159 @default.
• W2563939710 cites W1988528341 @default.
• W2563939710 cites W1988772771 @default.
• W2563939710 cites W1989288655 @default.
• W2563939710 cites W1989713934 @default.
• W2563939710 cites W1990247717 @default.
• W2563939710 cites W1998030591 @default.
• W2563939710 cites W2001931685 @default.
• W2563939710 cites W2002540268 @default.
• W2563939710 cites W2003128071 @default.
• W2563939710 cites W2005099086 @default.
• W2563939710 cites W2008897056 @default.
• W2563939710 cites W2013987160 @default.
• W2563939710 cites W2017244727 @default.
• W2563939710 cites W2021025164 @default.
• W2563939710 cites W2022168287 @default.
• W2563939710 cites W2022904816 @default.
• W2563939710 cites W2025980935 @default.
• W2563939710 cites W2028342041 @default.
• W2563939710 cites W2030810699 @default.
• W2563939710 cites W2033085732 @default.
• W2563939710 cites W2037478172 @default.
• W2563939710 cites W2038184434 @default.
• W2563939710 cites W2041183756 @default.
• W2563939710 cites W2042813819 @default.
• W2563939710 cites W2043403813 @default.
• W2563939710 cites W2052644995 @default.
• W2563939710 cites W2056082591 @default.
• W2563939710 cites W2056615483 @default.
• W2563939710 cites W2057045134 @default.
• W2563939710 cites W2057323262 @default.
• W2563939710 cites W2061509307 @default.
• W2563939710 cites W2067477118 @default.
• W2563939710 cites W2071453911 @default.
• W2563939710 cites W2075630485 @default.
• W2563939710 cites W2075781144 @default.
• W2563939710 cites W2077097585 @default.
• W2563939710 cites W2085678265 @default.
• W2563939710 cites W2089364767 @default.
• W2563939710 cites W2090879198 @default.
• W2563939710 cites W2090933028 @default.
• W2563939710 cites W2092215865 @default.
• W2563939710 cites W2094329484 @default.
• W2563939710 cites W2100900164 @default.
• W2563939710 cites W2102790268 @default.
• W2563939710 cites W2106052163 @default.
• W2563939710 cites W2107259349 @default.
• W2563939710 cites W2109996424 @default.
• W2563939710 cites W2111171021 @default.
• W2563939710 cites W2114710766 @default.
• W2563939710 cites W2116373834 @default.
• W2563939710 cites W2119688338 @default.
• W2563939710 cites W2122924553 @default.
• W2563939710 cites W2130017148 @default.
• W2563939710 cites W2134904666 @default.
• W2563939710 cites W2134924775 @default.
• W2563939710 cites W2143738823 @default.
• W2563939710 cites W2148506726 @default.
• W2563939710 cites W2288962623 @default.
• W2563939710 cites W2318719749 @default.
• W2563939710 cites W2330967458 @default.
• W2563939710 cites W2331568807 @default.
• W2563939710 cites W2341440047 @default.
• W2563939710 cites W2342695230 @default.
• W2563939710 cites W2499462499 @default.
• W2563939710 doi "https://doi.org/10.1144/jgs2016-056" @default.
• W2563939710 hasPublicationYear "2016" @default.
• W2563939710 type Work @default.
• W2563939710 sameAs 2563939710 @default.
• W2563939710 citedByCount "57" @default.
• W2563939710 countsByYear W25639397102017 @default.
• W2563939710 countsByYear W25639397102018 @default.
• W2563939710 countsByYear W25639397102019 @default.
• W2563939710 countsByYear W25639397102020 @default.
• W2563939710 countsByYear W25639397102021 @default.
• W2563939710 countsByYear W25639397102022 @default.
• W2563939710 countsByYear W25639397102023 @default.
• W2563939710 crossrefType "journal-article" @default.

• next