FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2332947981> ?p ?o ?g. }

• W2332947981 endingPage "16" @default.
• W2332947981 startingPage "3" @default.
• W2332947981 abstract "Calcite-filled extension veins and shear fractures are preserved in numerous travertine deposits along the western margin of the Albuquerque Basin of the Rio Grande rift. Calcite veins are banded and show geometries suggesting incremental cracking and calcite precipitation. U-series and 234U model ages from calcite infillings indicate that vein formation was active in the Quaternary, from ca. 2 Ma to ca. 250 ka. Vein orientations are systematic within each deposit and record a dominant extension direction that was horizontal and varied from E-W to NW-SE, consistent with both the regional finite extensional strain in the rift and with the global positioning system (GPS)–constrained deformation field. Three sites contain three orthogonal vein sets that crosscut one another nonsystematically, suggesting alternating times of: (1) regional E-W horizontal extension (dominant), (2) alternating N-S and E-W vertical veins that suggest vertical s1 and s2 » s3, and (3) horizontal veins that are interpreted to reflect times of highest pore fluid pressures and subequal principal stresses. One site contains conjugate normal faults that also record the dominant E-W extensional tectonic stress. Quaternary extensional strain rates calculated from vein opening for three locations range from 3.2 ± 1.4 × 10–16 s–1 to 3.2 × 10-15 ± 2.7 × 10–16 s–1, which are up to ∼40 times higher than the long-term (Oligocene–Holocene) finite strain rates calculated for different basins of the Rio Grande rift (8.5 × 10–17 to 4.5 × 10–16 s–1), and up to ∼100 times higher than modern strain rates measured by GPS data (3.9 × 10-17 ± 6.3 × 10–18 to 4.4 × 10-17 ± 6.3 × 10–18 s–1). These high Quaternary rates are comparable to modern strain rates measured in the Basin and Range Province and East African Rift. Thus, this paper documents persistent E-W regional extension through the Quaternary in the Rio Grande rift that bridges geologic, paleoseismic, and GPS rates. Anomalously high strain rates in the Quaternary were facilitated by ascent of travertine-depositing CO2-rich waters along rift-bounding normal faults, leading to locally very high stain accumulations. These sites also provide examples of natural leakage of deeply sourced CO2 interacting with regional tectonism, and they emphasize that rift maturation is a highly dynamic process, both spatially and temporally." @default.
• W2332947981 created "2016-06-24" @default.
• W2332947981 creator A5048707050 @default.
• W2332947981 creator A5069066250 @default.
• W2332947981 creator A5069337554 @default.
• W2332947981 creator A5069529201 @default.
• W2332947981 creator A5085099475 @default.
• W2332947981 creator A5090086069 @default.
• W2332947981 date "2014-02-01" @default.
• W2332947981 modified "2023-10-18" @default.
• W2332947981 title "Quaternary extension in the Rio Grande rift at elevated strain rates recorded in travertine deposits, central New Mexico" @default.
• W2332947981 cites W1651690650 @default.
• W2332947981 cites W1955520095 @default.
• W2332947981 cites W1963759171 @default.
• W2332947981 cites W1964132572 @default.
• W2332947981 cites W1975630028 @default.
• W2332947981 cites W1987728247 @default.
• W2332947981 cites W1988143821 @default.
• W2332947981 cites W1996586016 @default.
• W2332947981 cites W2003394091 @default.
• W2332947981 cites W2010395847 @default.
• W2332947981 cites W2012640099 @default.
• W2332947981 cites W2023017648 @default.
• W2332947981 cites W2026976482 @default.
• W2332947981 cites W2030778931 @default.
• W2332947981 cites W2032340360 @default.
• W2332947981 cites W2047475761 @default.
• W2332947981 cites W2053108236 @default.
• W2332947981 cites W2062616633 @default.
• W2332947981 cites W2072577786 @default.
• W2332947981 cites W2072585927 @default.
• W2332947981 cites W2094639876 @default.
• W2332947981 cites W2100187556 @default.
• W2332947981 cites W2100859764 @default.
• W2332947981 cites W2102069069 @default.
• W2332947981 cites W2118282237 @default.
• W2332947981 cites W2148871206 @default.
• W2332947981 cites W2150311903 @default.
• W2332947981 cites W2170569840 @default.
• W2332947981 cites W2274181520 @default.
• W2332947981 cites W2298012029 @default.
• W2332947981 cites W2339991708 @default.
• W2332947981 cites W2342564574 @default.
• W2332947981 cites W2396556479 @default.
• W2332947981 cites W2466477307 @default.
• W2332947981 cites W2724477917 @default.
• W2332947981 cites W4234440840 @default.
• W2332947981 cites W4293842629 @default.
• W2332947981 cites W4312585782 @default.
• W2332947981 doi "https://doi.org/10.1130/l278.1" @default.
• W2332947981 hasPublicationYear "2014" @default.
• W2332947981 type Work @default.
• W2332947981 sameAs 2332947981 @default.
• W2332947981 citedByCount "29" @default.
• W2332947981 countsByYear W23329479812014 @default.
• W2332947981 countsByYear W23329479812015 @default.
• W2332947981 countsByYear W23329479812016 @default.
• W2332947981 countsByYear W23329479812017 @default.
• W2332947981 countsByYear W23329479812018 @default.
• W2332947981 countsByYear W23329479812019 @default.
• W2332947981 countsByYear W23329479812020 @default.
• W2332947981 countsByYear W23329479812021 @default.
• W2332947981 countsByYear W23329479812022 @default.
• W2332947981 crossrefType "journal-article" @default.
• W2332947981 hasAuthorship W2332947981A5048707050 @default.
• W2332947981 hasAuthorship W2332947981A5069066250 @default.
• W2332947981 hasAuthorship W2332947981A5069337554 @default.
• W2332947981 hasAuthorship W2332947981A5069529201 @default.
• W2332947981 hasAuthorship W2332947981A5085099475 @default.
• W2332947981 hasAuthorship W2332947981A5090086069 @default.
• W2332947981 hasBestOaLocation W23329479811 @default.
• W2332947981 hasConcept C109007969 @default.
• W2332947981 hasConcept C114793014 @default.
• W2332947981 hasConcept C118552586 @default.
• W2332947981 hasConcept C127313418 @default.
• W2332947981 hasConcept C136137745 @default.
• W2332947981 hasConcept C140345934 @default.
• W2332947981 hasConcept C151730666 @default.
• W2332947981 hasConcept C15744967 @default.
• W2332947981 hasConcept C160464908 @default.
• W2332947981 hasConcept C165205528 @default.
• W2332947981 hasConcept C17409809 @default.
• W2332947981 hasConcept C2777202286 @default.
• W2332947981 hasConcept C2778471503 @default.
• W2332947981 hasConcept C2780191791 @default.
• W2332947981 hasConcept C50682988 @default.
• W2332947981 hasConcept C52678131 @default.
• W2332947981 hasConcept C5900021 @default.
• W2332947981 hasConcept C77928131 @default.
• W2332947981 hasConcept C96035792 @default.
• W2332947981 hasConceptScore W2332947981C109007969 @default.
• W2332947981 hasConceptScore W2332947981C114793014 @default.
• W2332947981 hasConceptScore W2332947981C118552586 @default.
• W2332947981 hasConceptScore W2332947981C127313418 @default.
• W2332947981 hasConceptScore W2332947981C136137745 @default.
• W2332947981 hasConceptScore W2332947981C140345934 @default.
• W2332947981 hasConceptScore W2332947981C151730666 @default.
• W2332947981 hasConceptScore W2332947981C15744967 @default.

• next