FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1984908630> ?p ?o ?g. }

• W1984908630 abstract "Summary -- The north-south-trending regionally significant Straight Creek Fault roughly bisects the Sauk River quadrangle and defines the fundamental geologic framework of it. Within the quadrangle, the Fault mostly separates low-grade metamorphic rocks on the west from medium- to high-grade metamorphic rocks of the Cascade metamorphic core. On the west, the Helena-Haystack melange and roughly coincident Darrington-Devils Mountain Fault Zone separate the western and eastern melange belts to the southwest from the Easton Metamorphic Suite, the Bell Pass melange, and rocks of the Chilliwack Group, to the northeast. The tectonic melanges have mostly Mesozoic marine components whereas the Chilliwack is mostly composed of Late Paleozoic arc rocks. Unconformably overlying the melanges and associated rocks are Eocene volcanic and sedimentary rocks, mostly infaulted along the Darrington-Devils Mountain Fault Zone. These younger rocks and a few small Eocene granitic plutons represent an extensional tectonic episode. East of the Straight Creek Fault, medium to high-grade regional metamorphic rocks of the Nason, Chelan Mountains, and Swakane terranes have been intruded by deep seated, Late Cretaceous granodioritic to tonalitic plutons, mostly now orthogneisses. Unmetamorphosed mostly tonalitic intrusions on both sides of the Straight Creek fault range from 35 to 4 million years old and represent the roots of volcanoes of the Cascade Magmatic Arc. Arc volcanic rocks are sparsely preserved east of the Straight Creek fault, but dormant Glacier Peak volcano on the eastern margin of the quadrangle is the youngest member of the Arc. Deposits of the Canadian Ice Sheet are well represented on the west side of the quadrangle, whereas alpine glacial deposits are common to the east. Roughly 5000 years ago lahars from Glacier Peak flowed westward filling major valleys across the quadrangle." @default.
• W1984908630 created "2016-06-24" @default.
• W1984908630 creator A5026089399 @default.
• W1984908630 creator A5031240197 @default.
• W1984908630 creator A5033095829 @default.
• W1984908630 creator A5072324722 @default.
• W1984908630 date "2002-01-01" @default.
• W1984908630 modified "2023-09-27" @default.
• W1984908630 title "Geologic map of the Sauk River 30- by 60-minute quadrangle, Washington" @default.
• W1984908630 cites W121870262 @default.
• W1984908630 cites W1485307181 @default.
• W1984908630 cites W1486033487 @default.
• W1984908630 cites W1532851400 @default.
• W1984908630 cites W1534756676 @default.
• W1984908630 cites W1542169830 @default.
• W1984908630 cites W154766908 @default.
• W1984908630 cites W1581080227 @default.
• W1984908630 cites W1586603461 @default.
• W1984908630 cites W1600222460 @default.
• W1984908630 cites W1608539236 @default.
• W1984908630 cites W1976989630 @default.
• W1984908630 cites W1979916163 @default.
• W1984908630 cites W1984121331 @default.
• W1984908630 cites W1992702913 @default.
• W1984908630 cites W1997881419 @default.
• W1984908630 cites W2001256002 @default.
• W1984908630 cites W2002000653 @default.
• W1984908630 cites W2006782784 @default.
• W1984908630 cites W2022533186 @default.
• W1984908630 cites W2031768666 @default.
• W1984908630 cites W2034414103 @default.
• W1984908630 cites W2039811736 @default.
• W1984908630 cites W2042829779 @default.
• W1984908630 cites W2044160890 @default.
• W1984908630 cites W2045845416 @default.
• W1984908630 cites W2046696482 @default.
• W1984908630 cites W2049031404 @default.
• W1984908630 cites W2059512314 @default.
• W1984908630 cites W2071946564 @default.
• W1984908630 cites W2072288277 @default.
• W1984908630 cites W2073428135 @default.
• W1984908630 cites W2076447745 @default.
• W1984908630 cites W2080187974 @default.
• W1984908630 cites W2082679394 @default.
• W1984908630 cites W2086172946 @default.
• W1984908630 cites W2087888055 @default.
• W1984908630 cites W2088910518 @default.
• W1984908630 cites W2102198833 @default.
• W1984908630 cites W2115119895 @default.
• W1984908630 cites W2122748439 @default.
• W1984908630 cites W2131582706 @default.
• W1984908630 cites W2134609326 @default.
• W1984908630 cites W2137544653 @default.
• W1984908630 cites W2138077145 @default.
• W1984908630 cites W2152725528 @default.
• W1984908630 cites W2160531430 @default.
• W1984908630 cites W2164286595 @default.
• W1984908630 cites W218951606 @default.
• W1984908630 cites W2237212196 @default.
• W1984908630 cites W2262703509 @default.
• W1984908630 cites W2280672120 @default.
• W1984908630 cites W2314232646 @default.
• W1984908630 cites W2317715245 @default.
• W1984908630 cites W2330992315 @default.
• W1984908630 cites W2796998301 @default.
• W1984908630 cites W2803434246 @default.
• W1984908630 cites W2808449074 @default.
• W1984908630 cites W2897983363 @default.
• W1984908630 cites W2902860621 @default.
• W1984908630 cites W2903933562 @default.
• W1984908630 cites W2917456392 @default.
• W1984908630 cites W292861768 @default.
• W1984908630 cites W2945131691 @default.
• W1984908630 cites W2952055358 @default.
• W1984908630 cites W316046976 @default.
• W1984908630 cites W37280461 @default.
• W1984908630 cites W646950498 @default.
• W1984908630 cites W833995888 @default.
• W1984908630 cites W965860682 @default.
• W1984908630 cites W2030417528 @default.
• W1984908630 doi "https://doi.org/10.3133/i2592" @default.
• W1984908630 hasPublicationYear "2002" @default.
• W1984908630 type Work @default.
• W1984908630 sameAs 1984908630 @default.
• W1984908630 citedByCount "4" @default.
• W1984908630 countsByYear W19849086302018 @default.
• W1984908630 crossrefType "report" @default.
• W1984908630 hasAuthorship W1984908630A5026089399 @default.
• W1984908630 hasAuthorship W1984908630A5031240197 @default.
• W1984908630 hasAuthorship W1984908630A5033095829 @default.
• W1984908630 hasAuthorship W1984908630A5072324722 @default.
• W1984908630 hasBestOaLocation W19849086301 @default.
• W1984908630 hasConcept C114793014 @default.
• W1984908630 hasConcept C120806208 @default.
• W1984908630 hasConcept C127313418 @default.
• W1984908630 hasConcept C136137745 @default.
• W1984908630 hasConcept C150999391 @default.
• W1984908630 hasConcept C151730666 @default.
• W1984908630 hasConcept C17409809 @default.
• W1984908630 hasConcept C175551986 @default.

• next