FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W22908227> ?p ?o ?g. }

• W22908227 endingPage "180" @default.
• W22908227 startingPage "143" @default.
• W22908227 abstract "Abstract The Sierra Madre Occidental (SMO) is the largest continuous ignimbrite province in the world. It covers the NW portion of Mexico and has a minimum estimated volcanic rock volume of about 400,000 km 3 . The southern part of the North American Basin and Range extensional province is in Mexico and was formed by NW- to NE-trending normal faults that bound many large grabens, which are particularly long and deep in the southern SMO. Graben formation and ignimbrite-forming pyroclastic flow eruptions coincided in space and time, particularly for the 38–23 Ma period, which has been referred to as the Ignimbrite Flare-up event. Geologic observations in the southern SMO indicate that the vents of several large-volume silicic ignimbrites were related to the graben master faults. We propose the new name “graben caldera” for this type of explosive-volcano-tectonic-collapse structure. The evidences for vent location of graben calderas include large pyroclastic dikes, co-ignimbrite lithic-lag breccias, and post-ignimbrite aligned rhyolitic domes and rhyolitic lava dikes. All these features are found along the graben caldera walls or on the graben's margins and thus were controlled by the main graben faults. Large-volume ignimbrite-forming eruptions occurred during graben collapse, usually through several vents along the graben caldera walls. Often, only part of the graben acted as a collapse caldera. In most cases, the downdropped blocks inside the collapsed segment of the graben have several distinct tilting directions, opposite to those caused by regular domino faulting (with tilting outwards from the graben's axis), indicating a chaotic collapse of blocks. This is interpreted as collapse of blocks during magma evacuation from an elongated and possibly batholith-sized magma chamber controlled by the regional extensional tectonics that existed under the collapsed segment of the graben. This collapse produced a piece-meal-like caldera confined within a graben. Generally, the pyroclastic dikes occur as discontinuous elongate lenses rather than regular tabular bodies. Usually, an elongated lava dome filled the vent and this totally covers the pre-existent pyroclastic dike, but in some cases the pyroclastic dike is exposed. Faulting and subsidence continued for several millions of years after the collapse and ignimbrite emplacement, displacing the intra-graben caldera products downward into the tectonic depression, but preserving or even intensifying the chaotic arrangement of the collapsed blocks. Fluvio-lacustrine continental deposits are generally found beneath and over the main and most voluminous ignimbrite, indicating that subsidence started before ignimbrite emplacement and graben collapse, and that continued after these events. In many cases the graben caldera vents are related to gold and silver hydrothermal mineralisation; thus understanding the relationship between ignimbrites, graben caldera vents, and fluvio-lacustrine deposits will be important for economic purposes." @default.
• W22908227 created "2016-06-24" @default.
• W22908227 creator A5003336690 @default.
• W22908227 creator A5004381189 @default.
• W22908227 creator A5014524448 @default.
• W22908227 creator A5072087847 @default.
• W22908227 creator A5082470073 @default.
• W22908227 date "2008-01-01" @default.
• W22908227 modified "2023-10-14" @default.
• W22908227 title "Chapter 4 The Ignimbrite Flare-Up and Graben Calderas of the Sierra Madre Occidental, Mexico" @default.
• W22908227 cites W1542673127 @default.
• W22908227 cites W1641796164 @default.
• W22908227 cites W1951784736 @default.
• W22908227 cites W1964841086 @default.
• W22908227 cites W1970353965 @default.
• W22908227 cites W1975219751 @default.
• W22908227 cites W1975799208 @default.
• W22908227 cites W1978803880 @default.
• W22908227 cites W1981393972 @default.
• W22908227 cites W1992568494 @default.
• W22908227 cites W1997529291 @default.
• W22908227 cites W1999286284 @default.
• W22908227 cites W2006475534 @default.
• W22908227 cites W2007520293 @default.
• W22908227 cites W2013519121 @default.
• W22908227 cites W2031428847 @default.
• W22908227 cites W2049161324 @default.
• W22908227 cites W2051299687 @default.
• W22908227 cites W2059907493 @default.
• W22908227 cites W2067112977 @default.
• W22908227 cites W2067654075 @default.
• W22908227 cites W2075043444 @default.
• W22908227 cites W2078418919 @default.
• W22908227 cites W2083966746 @default.
• W22908227 cites W2085513759 @default.
• W22908227 cites W2092243072 @default.
• W22908227 cites W2094892015 @default.
• W22908227 cites W2099559840 @default.
• W22908227 cites W2103151937 @default.
• W22908227 cites W2105461390 @default.
• W22908227 cites W2108641227 @default.
• W22908227 cites W2111003637 @default.
• W22908227 cites W2118195995 @default.
• W22908227 cites W2125295657 @default.
• W22908227 cites W2143650526 @default.
• W22908227 cites W2151173578 @default.
• W22908227 cites W2161665601 @default.
• W22908227 cites W2164341129 @default.
• W22908227 cites W2168077196 @default.
• W22908227 cites W2180510242 @default.
• W22908227 cites W2238016667 @default.
• W22908227 cites W2271584821 @default.
• W22908227 cites W2274487728 @default.
• W22908227 cites W2277431758 @default.
• W22908227 cites W2307479209 @default.
• W22908227 cites W2768978725 @default.
• W22908227 cites W32112289 @default.
• W22908227 cites W4242436551 @default.
• W22908227 cites W64945431 @default.
• W22908227 doi "https://doi.org/10.1016/s1871-644x(07)00004-6" @default.
• W22908227 hasPublicationYear "2008" @default.
• W22908227 type Work @default.
• W22908227 sameAs 22908227 @default.
• W22908227 citedByCount "29" @default.
• W22908227 countsByYear W229082272012 @default.
• W22908227 countsByYear W229082272013 @default.
• W22908227 countsByYear W229082272014 @default.
• W22908227 countsByYear W229082272015 @default.
• W22908227 countsByYear W229082272016 @default.
• W22908227 countsByYear W229082272017 @default.
• W22908227 countsByYear W229082272018 @default.
• W22908227 countsByYear W229082272019 @default.
• W22908227 countsByYear W229082272020 @default.
• W22908227 countsByYear W229082272021 @default.
• W22908227 countsByYear W229082272022 @default.
• W22908227 countsByYear W229082272023 @default.
• W22908227 crossrefType "book-chapter" @default.
• W22908227 hasAuthorship W22908227A5003336690 @default.
• W22908227 hasAuthorship W22908227A5004381189 @default.
• W22908227 hasAuthorship W22908227A5014524448 @default.
• W22908227 hasAuthorship W22908227A5072087847 @default.
• W22908227 hasAuthorship W22908227A5082470073 @default.
• W22908227 hasConcept C109007969 @default.
• W22908227 hasConcept C114793014 @default.
• W22908227 hasConcept C120806208 @default.
• W22908227 hasConcept C127313418 @default.
• W22908227 hasConcept C165205528 @default.
• W22908227 hasConcept C166839181 @default.
• W22908227 hasConcept C192241223 @default.
• W22908227 hasConcept C25822816 @default.
• W22908227 hasConcept C49708893 @default.
• W22908227 hasConceptScore W22908227C109007969 @default.
• W22908227 hasConceptScore W22908227C114793014 @default.
• W22908227 hasConceptScore W22908227C120806208 @default.
• W22908227 hasConceptScore W22908227C127313418 @default.
• W22908227 hasConceptScore W22908227C165205528 @default.
• W22908227 hasConceptScore W22908227C166839181 @default.
• W22908227 hasConceptScore W22908227C192241223 @default.

• next