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Journal Article
Published: 24 August 2021
Bulletin of the Seismological Society of America (2021) 111 (5): 2317–2333.
... the science and engineering communities with tools that can quantify surface rupture features more accurately. On‐the‐ground surveys and measurements are still critical, but surveys from small uninhabited aerial systems (sUAS, also known as drones) with onboard cameras can supplement those data...
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Journal Article
Published: 01 December 1913
Bulletin of the Seismological Society of America (1913) 3 (4): 221–226.
... (review) 94 I1 terremoto del 24 Gennaio, 1912 , nelle Isole Jonie e sua veloeita di propagazione (review) . . . . . . . . . . . . . . . . . . . . . 94 Allen, C. GReviews of three papers by Agamennone . . . . . . . . 93, 94 BalIore, Montessus de--The so-called luminous phenomena of earthquakes...
Journal Article
Published: 01 January 2021
Journal of Paleontology (2021) 95 (1): 141–153.
... each other all around. In addition, Aenigmaticumcrinus n. gen. has the anitaxis restricted to the calix, many interradial plates, presence of fixed brachials, uniserial arms, and basals forming most of the dorsal cup. Aenigmaticumcrinus n. gen. resembles members of Dimerocrinitidae...
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Journal Article
Published: 01 August 2007
The Canadian Mineralogist (2007) 45 (4): 751–773.
... ). Serpentine–tremolite –talc–chlorite-bearing rocks constitute the most abundant member of this sequence, with intercalation of banded iron-formation (oxide and silicate facies), graphite–pyrrhotite–pyrite-bearing metacherts and basaltic tuffs ( Brenner et al. 1990 ). The region was affected...
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Journal Article
Journal: Interpretation
Published: 26 June 2015
Interpretation (2015) 3 (3): SZ27–SZ39.
... component of the GBM workflow consists of building an appropriate rock model for each end member (sand and shale in this Gulf of Mexico example) and defining a mixing law for each layer to build the initial seismic velocity model to be used in tomography. In parallel, the basin modeling uncertainty...
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Journal Article
Journal: AAPG Bulletin
Published: 01 June 1982
AAPG Bulletin (1982) 66 (6): 750–774.
... is separated from the evaporites of the Ibura Member by 600 m of sandstone, conglomerates, dark-gray shales, and inclusions of halite ( Fig. 8 ). The Paripueira evaporites are considered to be of early Aptian age because they underlie the late Aptian Ibura evaporites and are separated from them by a thick...
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Journal Article
Published: 01 October 2010
Italian Journal of Geosciences (2010) 129 (3): 450–456.
... of carbonate resediments is likely located toward the NE. The Colle Trodo Formation follows with an abrupt contact. It has been subdivided in two members, from bottom to top: the Alberosa Member and the Maierà Member. The Alberosa Member is constituted by a well bedded alternation of calcareous and marly...
FIGURES
Journal Article
Journal: Economic Geology
Published: 01 March 2000
Economic Geology (2000) 95 (2): 405–427.
... Geologia , Goiânia, Goiás , 34th, Abstracts, v. 3 , p. 294 – 295 . Guimarães , D. , 1951 , Arquibrasil e sua evolução geológica. Brasil : Rio de Janeiro, Departamento Nacional Producão Mineral, Divisão do Fomento Produção Mineral, Boletim 88 , 314 p. Guimarães , D...
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Journal Article
Published: 15 June 2015
Geological Magazine (2016) 153 (1): 84–94.
.... & Di Celma C. 2011 . Taphonomic and paleoecological analyses (mollusks and fishes) of the Súa Member condensed shellbed, Upper Onzole Formation (Early Pliocene, Ecuador) . Palaios 26 , 160 –72. Chapman...
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Journal Article
Published: 01 July 2005
Journal of Paleontology (2005) 79 (4): 663–669.
... punctulatus istriensis was similar to members of both Harpactocarcinus and Harpactoxanthopsis . Via (1959) and Schweitzer (2003) discussed the differences between these two genera, the major difference being that species of Harpactoxanthopsis possess four well-developed anterolateral spines...
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Journal Article
Journal: Palynology
Published: 02 October 2018
Palynology (2018) 42 (4): 457–465.
... an important step in understanding more precisely the environmental shifts that occurred in the Quaternary in the Pantanal. The authors thank Cátia Nunes da Cunha and Ana Costa Dantas, members of the evaluation commission; and Germano Guarim Neto, curator of the central Herbarium of UFMT. We thank...
Journal Article
Journal: Clay Minerals
Published: 01 June 2013
Clay Minerals (2013) 48 (3): 473–480.
... , 28 , 731 – 735 . Delavi D.G.G. ( 2011 ) Defloculação de suspensões aquosas de argilas e sua correlação com caracterizações químicas e de superfícies . Dissertation . Federal University of Santa Catarina , Brazil . Dinger D.R. ( 2002 ) Rheology for ceramists , 213 pp...
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Journal Article
Published: 01 September 2011
Journal of Paleontology (2011) 85 (5): 877–881.
... discussed. 17 01 2011 2011 PODOCNEMIDOID TURTLES are formed, according to Gaffney et al., (2006) , by the two most diverse groups of pleurodires or side-necked turtles: the extinct Bothremydidae and the extant and fossil members of Podocnemididae plus Brasilemys josai Lapparent de...
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Journal Article
Published: 01 November 2006
Journal of Paleontology (2006) 80 (6): 1172–1178.
... , rather than species of Channa , and is here described as a new species, Parachanna fayumensis . It differs from the other species of the genus in possessing a prominent tooth patch on the posterior end of the parasphenoid. This new species of channid is the oldest member of the family known from Africa...
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Journal Article
Journal: The Leading Edge
Published: 01 April 2018
The Leading Edge (2018) 37 (4): 252–254.
... Argentina, two from Brazil, and one from Colombia. To lead off the special section, Acevedo and Bande present a seismic reservoir characterization study in which they estimate total organic carbon (TOC) values and brittleness for the lower members of the Vaca Muerta Formation, La Cocina and El Orgánico...
Journal Article
Journal: Palynology
Published: 01 January 2002
Palynology (2002) 26 (1): 135–165.
... was named by Evans (1894) . Melo (1988) re-validated and informally subdivided the Chapada Group into units 1–4, corresponding to the units described by Andrade and Camarço (1980 , 1982) . This approach was followed by Grahn (1992) . However, it is controversial if the middle member of the Ponta...
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Journal Article
Published: 01 July 2006
Seismological Research Letters (2006) 77 (4): 453–459.
... of natural hazards. Experts within the group include seismologists, geophysicists, mathematicians, structural engineers, software engineers, economists, and social scientists. The work has benefited greatly from collaboration with members of the global re-insurance sector, something that also was encouraged...
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Journal Article
Journal: PALAIOS
Published: 27 February 2018
PALAIOS (2018) 33 (2): 69–84.
... was identified by Cazzulo-Klepzig (1979) at the top of the Serrinha Member's type-section (in the Lauro Müller–São Joaquim highway, km 19, Santa Catarina State). Above this level, an intraformational breccia indicates the erosive contact between the Serrinha and the overlying Morro Pelado Member. Moreover, we...
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Journal Article
Journal: Palynology
Published: 01 January 2000
Palynology (2000) 24 (1): 147–176.
... ., and thus of late Emsian age. The Tibaji is here considered as a member of the Ponta Grossa Formation sensu Oliveira (1912) . The lowermost part of the São Domingos Formation, as defined by Maack (1947) at the same type locality as for the Tibaji Member, is considered late Emsian. Lithologically...
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Journal Article
Journal: GSA Bulletin
Published: 01 January 2014
GSA Bulletin (2014) 126 (3-4): 459–480.
... deposits, backed by paleo-lagoon and washover sequences, and fronted by a welded regressive strandplain ( Villwock et al., 1986 ; Martin et al., 1988 ; Dillenburg et al., 2004 , 2009 ). The four late-stage transgressive-highstand deposit types described herein are end-members along a continuum...
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