FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2076753875> ?p ?o ?g. }

• W2076753875 endingPage "473" @default.
• W2076753875 startingPage "449" @default.
• W2076753875 abstract "While relatively rapid and large‐scale extension occurred in the Death Valley region of California during Neogene time, little or no shallow extension occurred in the adjacent Sierra Nevada. This contrast in tectonic history has often been extrapolated to include the entire lithosphere, but geophysical and geologic observations indicate that more extension of the mantle lithosphere has occurred under the Sierra than under the Death Valley region. Upper mantle seismic velocities observed beneath the High Sierra are lower than those observed in other regions with comparable surface heat flow. This discrepancy could be resolved if the mantle lithosphere beneath the High Sierra had become warmer, presumably by tectonic thinning, in the last 10 m.y. Upper mantle seismic velocities, averaged topography, and Bouguer gravity anomalies all are consistent with the presence of thinner mantle lithosphere beneath the High Sierra than beneath the California portion of the Basin and Range Province to the east. This suggests that extension of the crust near Death Valley might be accommodated at a deeper level by thinning of the mantle lithosphere beneath the Sierra Nevada. The extension in the crust of the California Basin and Range Province and the thinning of the mantle lithosphere under the High Sierra appear to share the same bounds in time and space. The uplift of the High Sierra occurred over the past 9 m.y., which coincides with most of the extension that occurred in the California Basin and Range Province. Because the orientation of extension in the California Basin and Range Province is inferred to be approximately N60°W from geologic, geodetic, and in situ stress measurements, the northern and southern edges of the Death Valley extensional subprovince may extend N60°W from the inferred northern and southern limits of west dipping low‐angle normal faults of the Death Valley region. Pronounced changes in the averaged topography and Bouguer gravity anomaly across these two bounds both in the Basin and Range Province and in the Sierra Nevada support a connection between the tectonics of both regions. The geomorphic history of the southern Sierra suggests an up‐to‐the‐north warp of the Sierra across this southern bound during latest Cenozoic time. Hence extension near Death Valley may be localized in the crust and may be laterally connected to thinning of the mantle lithosphere beneath the Sierra Nevada. This geometry requires." @default.
• W2076753875 created "2016-06-24" @default.
• W2076753875 creator A5042026351 @default.
• W2076753875 date "1987-08-01" @default.
• W2076753875 modified "2023-09-27" @default.
• W2076753875 title "Is extension in Death Valley accommodated by thinning of the mantle lithosphere beneath the Sierra Nevada, California?" @default.
• W2076753875 cites W119019604 @default.
• W2076753875 cites W1492942587 @default.
• W2076753875 cites W1495750695 @default.
• W2076753875 cites W1598222017 @default.
• W2076753875 cites W17255637 @default.
• W2076753875 cites W1839082771 @default.
• W2076753875 cites W1860864598 @default.
• W2076753875 cites W1903458979 @default.
• W2076753875 cites W1967259368 @default.
• W2076753875 cites W1972167093 @default.
• W2076753875 cites W1974029746 @default.
• W2076753875 cites W1974109556 @default.
• W2076753875 cites W1976079867 @default.
• W2076753875 cites W1980139688 @default.
• W2076753875 cites W1981155537 @default.
• W2076753875 cites W1981938499 @default.
• W2076753875 cites W1982312509 @default.
• W2076753875 cites W1985274054 @default.
• W2076753875 cites W1987008432 @default.
• W2076753875 cites W1987841795 @default.
• W2076753875 cites W1988763862 @default.
• W2076753875 cites W1988915166 @default.
• W2076753875 cites W1997189140 @default.
• W2076753875 cites W1999128011 @default.
• W2076753875 cites W2007717178 @default.
• W2076753875 cites W2007849908 @default.
• W2076753875 cites W2008112980 @default.
• W2076753875 cites W2008948116 @default.
• W2076753875 cites W2014406468 @default.
• W2076753875 cites W2015263471 @default.
• W2076753875 cites W2018190396 @default.
• W2076753875 cites W2021440632 @default.
• W2076753875 cites W2024625702 @default.
• W2076753875 cites W2025640210 @default.
• W2076753875 cites W2031092702 @default.
• W2076753875 cites W2031768666 @default.
• W2076753875 cites W2036108179 @default.
• W2076753875 cites W2039243568 @default.
• W2076753875 cites W2041156213 @default.
• W2076753875 cites W2041698640 @default.
• W2076753875 cites W2048088930 @default.
• W2076753875 cites W2049633774 @default.
• W2076753875 cites W2052685439 @default.
• W2076753875 cites W2066994889 @default.
• W2076753875 cites W2074991281 @default.
• W2076753875 cites W2075420246 @default.
• W2076753875 cites W2086303149 @default.
• W2076753875 cites W2092118088 @default.
• W2076753875 cites W2097515808 @default.
• W2076753875 cites W2105299011 @default.
• W2076753875 cites W2106467454 @default.
• W2076753875 cites W2110053897 @default.
• W2076753875 cites W2110171251 @default.
• W2076753875 cites W2113605026 @default.
• W2076753875 cites W2124474119 @default.
• W2076753875 cites W2130897619 @default.
• W2076753875 cites W2132269632 @default.
• W2076753875 cites W2139732287 @default.
• W2076753875 cites W2139864345 @default.
• W2076753875 cites W2139928701 @default.
• W2076753875 cites W2144130121 @default.
• W2076753875 cites W2147618298 @default.
• W2076753875 cites W2147959855 @default.
• W2076753875 cites W2151394593 @default.
• W2076753875 cites W2154571633 @default.
• W2076753875 cites W2155500845 @default.
• W2076753875 cites W2271135478 @default.
• W2076753875 cites W2330214787 @default.
• W2076753875 cites W2380374024 @default.
• W2076753875 cites W2399252851 @default.
• W2076753875 cites W25561617 @default.
• W2076753875 cites W2578364624 @default.
• W2076753875 cites W2584461937 @default.
• W2076753875 cites W63076898 @default.
• W2076753875 cites W78869628 @default.
• W2076753875 doi "https://doi.org/10.1029/tc006i004p00449" @default.
• W2076753875 hasPublicationYear "1987" @default.
• W2076753875 type Work @default.
• W2076753875 sameAs 2076753875 @default.
• W2076753875 citedByCount "50" @default.
• W2076753875 countsByYear W20767538752012 @default.
• W2076753875 countsByYear W20767538752013 @default.
• W2076753875 countsByYear W20767538752014 @default.
• W2076753875 countsByYear W20767538752015 @default.
• W2076753875 countsByYear W20767538752017 @default.
• W2076753875 countsByYear W20767538752020 @default.
• W2076753875 countsByYear W20767538752021 @default.
• W2076753875 crossrefType "journal-article" @default.
• W2076753875 hasAuthorship W2076753875A5042026351 @default.
• W2076753875 hasConcept C109007969 @default.
• W2076753875 hasConcept C127313418 @default.
• W2076753875 hasConcept C151730666 @default.

• next