FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2804656588> ?p ?o ?g. }

• W2804656588 endingPage "41" @default.
• W2804656588 startingPage "27" @default.
• W2804656588 abstract "Abstract Investigation of large scale suture zones in old continental interiors offers insights into the evolution of continents. The Dharwar Craton (DC) and the Southern Granulite Terrain(SGT) of the Indian shield represent large segments of Precambrian middle to lower crust and preserve a geological record spanning from Mesoarchean to Cambrian. This study illuminates the deep structure of the Palghat-Cauvery Shear Zone System (PCSS) and the Palghat-Cauvery Suture Zone (PCSZ) that comprise crustal-scale structures related to multiple episodes of orogeny, crust formation and reworking. We utilize here 3202 high quality P-receiver functions computed using new data from a 23 station seismic network operated by us. Results show a thick (>38 km) mafic (Poisson's ratio >0.25) crust beneath the SGT. The change in crustal thickness is gradual, with a shallower Moho towards the south of PCSZ. We found little evidence for drastic changes in crustal thickness across prominent shear zones like the PCSZ and Moyar-Bhavani. Few seismic stations located along these boundaries have shown evidence for dipping reflectors around 8–20 km depth, with strikes matching well with the trends of surface geological sutures. We opine that these suture zones do not show indications of a terrane boundary. However, a drastic change in the crustal thickness is observed around the prograde metamorphic transition zone or broadly, the “Fermor line”, which separates rocks of Chanockitic (Orthopyroxene bearing granitoid) and non-Charnockitic (Orthopyroxene-free granitoid) mineral assemblage, further north beneath the DC. We suggest that thicknening of crust north of Moyar-Attur Shear Zone (MASZ) and around Fermor line is related to subduction processes operative during the Precambrian." @default.
• W2804656588 created "2018-06-01" @default.
• W2804656588 creator A5000320359 @default.
• W2804656588 creator A5032466790 @default.
• W2804656588 creator A5035167715 @default.
• W2804656588 creator A5056568681 @default.
• W2804656588 creator A5063316809 @default.
• W2804656588 creator A5085814458 @default.
• W2804656588 date "2018-08-01" @default.
• W2804656588 modified "2023-09-27" @default.
• W2804656588 title "Vestiges of Precambrian subduction in the south Indian shield? - A seismological perspective" @default.
• W2804656588 cites W1704501138 @default.
• W2804656588 cites W1827757642 @default.
• W2804656588 cites W1965679011 @default.
• W2804656588 cites W1967185069 @default.
• W2804656588 cites W1971844979 @default.
• W2804656588 cites W1971892298 @default.
• W2804656588 cites W1972319641 @default.
• W2804656588 cites W1973310819 @default.
• W2804656588 cites W1973439798 @default.
• W2804656588 cites W1975871169 @default.
• W2804656588 cites W1978567788 @default.
• W2804656588 cites W1980788306 @default.
• W2804656588 cites W1982712732 @default.
• W2804656588 cites W1983971237 @default.
• W2804656588 cites W1984297449 @default.
• W2804656588 cites W1985925759 @default.
• W2804656588 cites W1989676536 @default.
• W2804656588 cites W1997745935 @default.
• W2804656588 cites W2000273636 @default.
• W2804656588 cites W2001820253 @default.
• W2804656588 cites W2012822419 @default.
• W2804656588 cites W2012976943 @default.
• W2804656588 cites W2023893845 @default.
• W2804656588 cites W2024791415 @default.
• W2804656588 cites W2025841258 @default.
• W2804656588 cites W2028864600 @default.
• W2804656588 cites W2029434609 @default.
• W2804656588 cites W2030397687 @default.
• W2804656588 cites W2036078919 @default.
• W2804656588 cites W2039413021 @default.
• W2804656588 cites W2044552515 @default.
• W2804656588 cites W2047559336 @default.
• W2804656588 cites W2056155689 @default.
• W2804656588 cites W2060293298 @default.
• W2804656588 cites W2063762553 @default.
• W2804656588 cites W2066755614 @default.
• W2804656588 cites W2068132931 @default.
• W2804656588 cites W2072741237 @default.
• W2804656588 cites W2079993608 @default.
• W2804656588 cites W2081516882 @default.
• W2804656588 cites W2083266769 @default.
• W2804656588 cites W2087611505 @default.
• W2804656588 cites W2088284794 @default.
• W2804656588 cites W2089778945 @default.
• W2804656588 cites W2132509829 @default.
• W2804656588 cites W2142857241 @default.
• W2804656588 cites W2145160948 @default.
• W2804656588 cites W2145729420 @default.
• W2804656588 cites W2147711068 @default.
• W2804656588 cites W2157271226 @default.
• W2804656588 cites W2158587999 @default.
• W2804656588 cites W2164602066 @default.
• W2804656588 cites W2166251787 @default.
• W2804656588 cites W2171746390 @default.
• W2804656588 cites W2174216460 @default.
• W2804656588 cites W2258351827 @default.
• W2804656588 cites W2295186625 @default.
• W2804656588 cites W2362392717 @default.
• W2804656588 cites W2885542573 @default.
• W2804656588 cites W4233438985 @default.
• W2804656588 doi "https://doi.org/10.1016/j.tecto.2018.05.005" @default.
• W2804656588 hasPublicationYear "2018" @default.
• W2804656588 type Work @default.
• W2804656588 sameAs 2804656588 @default.
• W2804656588 citedByCount "5" @default.
• W2804656588 countsByYear W28046565882020 @default.
• W2804656588 countsByYear W28046565882021 @default.
• W2804656588 countsByYear W28046565882023 @default.
• W2804656588 crossrefType "journal-article" @default.
• W2804656588 hasAuthorship W2804656588A5000320359 @default.
• W2804656588 hasAuthorship W2804656588A5032466790 @default.
• W2804656588 hasAuthorship W2804656588A5035167715 @default.
• W2804656588 hasAuthorship W2804656588A5056568681 @default.
• W2804656588 hasAuthorship W2804656588A5063316809 @default.
• W2804656588 hasAuthorship W2804656588A5085814458 @default.
• W2804656588 hasConcept C12713177 @default.
• W2804656588 hasConcept C127313418 @default.
• W2804656588 hasConcept C138081364 @default.
• W2804656588 hasConcept C147717901 @default.
• W2804656588 hasConcept C151730666 @default.
• W2804656588 hasConcept C165205528 @default.
• W2804656588 hasConcept C173776410 @default.
• W2804656588 hasConcept C2524010 @default.
• W2804656588 hasConcept C2775973192 @default.
• W2804656588 hasConcept C33923547 @default.
• W2804656588 hasConcept C58097730 @default.
• W2804656588 hasConcept C77928131 @default.

• next