FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4220783337> ?p ?o ?g. }

• W4220783337 endingPage "103768" @default.
• W4220783337 startingPage "103768" @default.
• W4220783337 abstract "The Calmallí (CA), Piedra Blanca (PB), and El Barril (EB) plutons were emplaced during the Late Cretaceous at the southern limit of the Peninsular Ranges batholith (PRB) at the present latitude of ∼28°N. These plutonic suites are juxtaposed, showing contrasting compositions, probably associated with different basement rocks. The region is separated by the high magnetic values in the western zone compared with the lowest magnetic values in the eastern zone. The western CA pluton intrudes a Jurassic island arc assemblage, whereas host rocks outcrops of the PB and EB are absent, but it is inferred that they intruded into the eastern margin of the Jurassic arc. The CA plutonic suite has a ca. 100 Ma old mafic core surrounded by ca. 102–105 Ma old tonalities. Such zonation is a typical feature of many plutons of the western PRB. The PB and EB plutons show granodioritic to granitic compositions of ca. 92 Ma. We compare the paleoposition of the CA-EB section with respect to the San José, and San Pedro Mártir plutons (∼31°N), and the Compostela pluton (∼29°N) which yield clockwise rotations of 31°–45°, and 16.4°, respectively. These northern plutons record rotations by tectonic deformation at suture zones between the Alisitos island arc and the older North America craton. Based on the paleomagnetic observations in the transition zone between western and eastern type plutons, we analyzed 15 sites from the CA, nine from the PB, and 23 from EB to evaluate their paleoposition. We obtained the characteristic remanent magnetizations (ChRM) following the detailed stepwise alternating magnetic field (AF) and thermal demagnetization methods. Each pluton was compared to the reference pole of North America at 100 Ma and 90 Ma. The paleopoles do not differ much from the cratonic references since the data indicate an apparent clockwise rotation of 8.1° ± 8.8° and a flattening of −13.9° ± 10.6° for CA pluton and an apparent clockwise rotation of 1.43° ± 8.3° and −14.2° ± 9.8° of flattening for combined paleopole of PB and EB plutons. Statistically, the paleopoles displacement are not significative, similar to five cretaceous plutons located NNW of the study area, suggesting that the mid-Cretaceous plutonic suites of the southern PRB remained stable since their emplacement in a period between 128 Ma and 90 Ma." @default.
• W4220783337 created "2022-04-03" @default.
• W4220783337 creator A5016453192 @default.
• W4220783337 creator A5049036658 @default.
• W4220783337 creator A5055314203 @default.
• W4220783337 creator A5081979102 @default.
• W4220783337 creator A5084856921 @default.
• W4220783337 date "2022-04-01" @default.
• W4220783337 modified "2023-10-17" @default.
• W4220783337 title "Apparent undisturbed paleoposition of mid-Cretaceous plutons emplaced across a Jurassic island arc segment in the southernmost part of the Peninsular Ranges batholith, Baja California, Mexico" @default.
• W4220783337 cites W1637912772 @default.
• W4220783337 cites W1969447332 @default.
• W4220783337 cites W1977063213 @default.
• W4220783337 cites W1977308170 @default.
• W4220783337 cites W1980364678 @default.
• W4220783337 cites W1980529905 @default.
• W4220783337 cites W1981752220 @default.
• W4220783337 cites W2019034794 @default.
• W4220783337 cites W2021987309 @default.
• W4220783337 cites W2025441376 @default.
• W4220783337 cites W2033475216 @default.
• W4220783337 cites W2036047077 @default.
• W4220783337 cites W2052436256 @default.
• W4220783337 cites W2057794589 @default.
• W4220783337 cites W2059099764 @default.
• W4220783337 cites W2059603619 @default.
• W4220783337 cites W2063421616 @default.
• W4220783337 cites W2075940125 @default.
• W4220783337 cites W2080460062 @default.
• W4220783337 cites W2095800081 @default.
• W4220783337 cites W2103999221 @default.
• W4220783337 cites W2116389071 @default.
• W4220783337 cites W2118204502 @default.
• W4220783337 cites W2121812998 @default.
• W4220783337 cites W2130851188 @default.
• W4220783337 cites W2145398453 @default.
• W4220783337 cites W2154610467 @default.
• W4220783337 cites W2206808472 @default.
• W4220783337 cites W2306789206 @default.
• W4220783337 cites W2330476109 @default.
• W4220783337 cites W2344784084 @default.
• W4220783337 cites W2412698757 @default.
• W4220783337 cites W2472883058 @default.
• W4220783337 cites W2522031466 @default.
• W4220783337 cites W2525674289 @default.
• W4220783337 cites W2755847301 @default.
• W4220783337 cites W2889855710 @default.
• W4220783337 cites W3021104574 @default.
• W4220783337 cites W3037259555 @default.
• W4220783337 cites W3185851872 @default.
• W4220783337 doi "https://doi.org/10.1016/j.jsames.2022.103768" @default.
• W4220783337 hasPublicationYear "2022" @default.
• W4220783337 type Work @default.
• W4220783337 citedByCount "0" @default.
• W4220783337 crossrefType "journal-article" @default.
• W4220783337 hasAuthorship W4220783337A5016453192 @default.
• W4220783337 hasAuthorship W4220783337A5049036658 @default.
• W4220783337 hasAuthorship W4220783337A5055314203 @default.
• W4220783337 hasAuthorship W4220783337A5081979102 @default.
• W4220783337 hasAuthorship W4220783337A5084856921 @default.
• W4220783337 hasConcept C12294951 @default.
• W4220783337 hasConcept C127313418 @default.
• W4220783337 hasConcept C151730666 @default.
• W4220783337 hasConcept C167284885 @default.
• W4220783337 hasConcept C172660882 @default.
• W4220783337 hasConcept C17409809 @default.
• W4220783337 hasConcept C180870510 @default.
• W4220783337 hasConcept C34122518 @default.
• W4220783337 hasConcept C58097730 @default.
• W4220783337 hasConcept C63379926 @default.
• W4220783337 hasConcept C77928131 @default.
• W4220783337 hasConceptScore W4220783337C12294951 @default.
• W4220783337 hasConceptScore W4220783337C127313418 @default.
• W4220783337 hasConceptScore W4220783337C151730666 @default.
• W4220783337 hasConceptScore W4220783337C167284885 @default.
• W4220783337 hasConceptScore W4220783337C172660882 @default.
• W4220783337 hasConceptScore W4220783337C17409809 @default.
• W4220783337 hasConceptScore W4220783337C180870510 @default.
• W4220783337 hasConceptScore W4220783337C34122518 @default.
• W4220783337 hasConceptScore W4220783337C58097730 @default.
• W4220783337 hasConceptScore W4220783337C63379926 @default.
• W4220783337 hasConceptScore W4220783337C77928131 @default.
• W4220783337 hasFunder F4320321739 @default.
• W4220783337 hasFunder F4320329453 @default.
• W4220783337 hasFunder F4320334834 @default.
• W4220783337 hasLocation W42207833371 @default.
• W4220783337 hasOpenAccess W4220783337 @default.
• W4220783337 hasPrimaryLocation W42207833371 @default.
• W4220783337 hasRelatedWork W129549350 @default.
• W4220783337 hasRelatedWork W1982349248 @default.
• W4220783337 hasRelatedWork W2000019012 @default.
• W4220783337 hasRelatedWork W2015916774 @default.
• W4220783337 hasRelatedWork W2068329156 @default.
• W4220783337 hasRelatedWork W2089278759 @default.
• W4220783337 hasRelatedWork W2122922600 @default.
• W4220783337 hasRelatedWork W4220783337 @default.
• W4220783337 hasRelatedWork W4311944423 @default.
• W4220783337 hasRelatedWork W2527038553 @default.

• next