Faulting within the San Juan–southern Gulf Islands Archipelagos, upper plate deformation of the Cascadia subduction complex

2020 ◽  
pp. SP505-2019-125
Author(s):  
H. Gary Greene ◽  
J. Vaughn Barrie
Keyword(s):  
San Juan ◽  
Plate Deformation ◽  
Gulf Islands

Turonian (Upper Cretaceous) lithostratigraphy and biochronology, southern Gulf Islands, British Columbia, and northern San Juan Islands, Washington State

2005 ◽  
Vol 42 (11) ◽  
pp. 2001-2020 ◽  
Author(s):  
James W Haggart ◽  
Peter D Ward ◽  
William Orr
Keyword(s):  
British Columbia ◽  
Washington State ◽  
San Juan ◽  
Submarine Fan ◽  
Island Formation ◽  
Shallow Marine ◽  
San Juan Islands ◽  
Thrust System ◽  
Gulf Islands ◽  
Facies Succession

Clastic strata preserved on Sidney Island, Barnes Island, and adjacent islands of the southernmost Gulf Islands of British Columbia and the northern San Juan Islands of Washington State are assigned to new stratigraphic units: the Sidney Island Formation and the Barnes Island Formation. The Sidney Island Formation consists of basal conglomerate and sandstone that grades upward through planar-stratified sandstone into hummocky cross-stratified sandstone and siltstone, all of which are deposited in relatively shallow-marine environments. The Barnes Island Formation, in contrast, consists of deep-marine conglomerate, sandstone, and mudstone that was deposited in a submarine-fan setting. Mollusk fossils from the Sidney Island Formation are of Early to Middle Turonian age, whereas ammonites and foraminifers from the Barnes Island Formation indicate a Late Turonian age. The Sidney Island Formation thus records initial marine transgression and inundation of basement rocks, followed by basin deepening that is transitional to the deep-marine submarine-fan deposits of the Barnes Island Formation. Sidney Island Formation strata have been considered previously as derived from uplift along the nearby San Juan thrust system in mid-Cretaceous time. However, the shallow-marine strata are internally well organized, and the facies succession is persistent across the formation's outcrop area. In addition, the formation lacks the distinctive detrital metamorphic mineral assemblages that are characteristic of older rocks of the San Juan Islands. These observations suggest that strata of the Sidney Island Formation did not accumulate immediately adjacent to active thrusting but rather in a more distal setting relative to the thrust system.

CASCADIA UPPER PLATE FAULTING IN THE SAN JUAN-SOUTH GULF ISLANDS ARCHIPELAGOS

2017 ◽  
Author(s):  
H. Gary Greene ◽  
◽  
Vaughn Barrie ◽  
Brian J. Todd ◽  
Kim Conway
Keyword(s):  
San Juan ◽  
Gulf Islands

scholarly journals Shaded seafloor relief, southern Gulf Islands and San Juan Archipelago, Canada and U.S.A.

2010 ◽  
Author(s):  
C Endris ◽  
K Picard ◽  
K G Greene ◽  
J V Barrie
Keyword(s):  
San Juan ◽  
Gulf Islands

Variabilidad genética de características morfológicas de maiz nativo (Zea mays L.) en la Península de Yucatán, México

2019 ◽  
Vol 12 (11) ◽  
Author(s):  
Antonio Villalobos-González ◽  
Mónica B. López-Hernández ◽  
Noel A. Valdivia-González ◽  
Enrique Arcocha-Gómez ◽  
Juan Medina-Méndez
Keyword(s):  
Zea Mays ◽  
Zea Mays L ◽  
San Juan

El objetivo fue estudiar la variabilidad genética de características morfológicas de maíces nativos en la Península de Yucatán (PY), México. Se utilizaron trece accesiones de maíz nativo reconocidas con el nombre de Naál Xóy, Xnúc Naál Blanco, Gallito Amarillo, Dzit Bacal, Mejeén Naál, Rosa San Juan, Cháck-Chóp, Teél Cháck, Sáck Teél, San Pableño, Ejú-Criollo Morado, Xmején Naál Tsitbacal y Clavo Chiapaneco. Los materiales se establecieron en Junio de 2017 y 2018, en Poxyaxum, Campeche, México, (19° 41´58.4´´ N, 90° 21´03.6´´ W y 30 msnm) bajo un diseño de bloques completos al azar con tres repeticiones. Los resultados revelaron diferencias (P£0.05) en las variables morfológicas evaluadas: número de días a floración masculina (FM) y femenina (FF) presento una inestabilidad de 12 días a FM y FF, con Naál Xóy y Ejú-Criollo Morado, y 15 días a madurez fisiológica con Clavo Chiapaneco. Una diferenciación de 98 y 126 cm en altura de mazorca y planta con Eju-Criollo Morado; 6 y 1.1 cm en longitud y diámetro de mazorca con Xnúc Naál Blanco y Cháck-Chóp, y Gallito Amarillo. Una variación de 4 hileras con Teél Cháck y 17 granos por hilera con San Pableño; 11 y 74 gr en peso de 100 granos (Xmején Naál Tsitbacal, Rosa San Juan y San Pableño) y granos por mazorca (Naál Xóy); y una diferencia mayor en rendimiento con Naál Xóy y Dzit Bacal de 3105 kg.ha-1.

Examen de ingenios, de Juan Huarte de San Juan, y los albores de la Neurobiología de la inteligencia en el Renacimiento español

2004 ◽  
Vol 38 (12) ◽  
pp. 1176 ◽  
Author(s):  
Antonio Martín Araguz ◽  
Cristina Bustamante Martínez
Keyword(s):  
San Juan
Sign in / Sign up

Export Citation Format

Share Document