30,792 research outputs found
Student Author- Andres Castillo, March 26, 2024
No full textFayetteville State University student author Andres Castillo speaks at the Chesnutt Library of Fayetteville State University about his book My Life Journey with Autism as a Military Child.
Presented live on March 26, 2024 as part of Chesnutt Library\u27s Faculty Author Series.https://digitalcommons.uncfsu.edu/faculty_author/1006/thumbnail.jp
Interview with Andres Martinez
No full textAuthor, Andres Martinez, discusses his dissertation and the resulting book he is writing that will expand on Valley conjunto musicians.https://scholarworks.utrgv.edu/bordermusicoralhistories/1014/thumbnail.jp
Kataloghaus: SISTEMA M ́HOUSE
No full textPresentazione del Prototipo Maisons M ́house di abitazione industriale in la revista D ́A di amplia diffusione architetturale.
Referimiento:
JANSER, Andres: “Kataloghaus
Revista Architese n. 1, Zurich, 1998
Pags. 34 y 35
Germano e ingles
Baker, Minnie M.
No full textLetter to Miss Baker from William M. Andres, Executive Director of the Oklahoma Arts and Humanities Council, Jan. 31, 1974. Mr. Andres thanks Miss Baker for her letter and interest in the Oklahoma Arts and Humanities Council
Parschisturella simplex Andres 1983
No full textParschisturella simplex Andres, 1983 Parschisturella simplex Andres, 1983: 213, figs 13, 14.— Barnard & Karaman, 1991: 517.— De Broyer & Jażdżewski, 1993: 74.— De Broyer et al., 2007: 165. Types. Holotype, male, 16 mm, ZMH K 32410. Paratype, male 20.3 mm ZMH K 32411. Type-locality. South Georgia, Walther Herwig 1977-78, sta. 492, (55°00’S 35°30’W), 0–120 m depth. Habitat. Marine. Depth range. 0–120 m. Feeding strategies. Not recorded. Remarks. See remarks under Parschisturella martrudan. Distribution. Southern Ocean. South Georgia (Andres 1983).Published as part of Lowry, J. K. & Kilgallen, N. M., 2014, A generic review of the lysianassoid family Uristidae and descriptions of new taxa from Australian waters (Crustacea, Amphipoda, Uristidae), pp. 1-92 in Zootaxa 3867 (1) on page 61, DOI: 10.11646/zootaxa.3867.1.1, http://zenodo.org/record/558573
Pseudfoxiphalus setosus Andres 1991
No full textPseudfoxiphalus setosus Andres, 1991 Andres, 1991: 187–196, figs. 1–5. De Broyer and JaŻdŻewski, 1993: 85. De Broyer and Rauschert, 1999: 286. Distribution: M Magellan Area: Chile, Seno de Reloncavi, Bahía Quillaipe, 41 ° 54 ’S 72 ° 75 ’W (sandy tidal flat) (HGA 91). Depth range: 0 m. Type-locality: Magellan Area: Chile, Seno de Reloncavi, Bahía Quillaipe, 41 ° 54 ’S 72 ° 75 ’W (sandy tidal flat) (HGA 91). Ecology: Collected from sandy tidal flat. Type material location: ZMH, Hamburg. Remarks: Since Andres (1991) described and illustrated the genus Pseudfoxiphalus, no other records or species were found.Published as part of Alonso, Gloria M., Pina, De, Rauschert, Martin & Broyer, Claude De, 2008, A catalogue of the Antarctic and sub-Antarctic Phoxocephalidae (Crustacea: Amphipoda: Gammaridea) with taxonomic, distribution and ecological data, pp. 1-40 in Zootaxa 1752 on page 27, DOI: 10.5281/zenodo.18174
Pseudfoxiphalus setosus Andres 1991
No full textPseudfoxiphalus setosus Andres, 1991 Andres, 1991: 187–196, figs. 1–5. De Broyer and JaŻdŻewski, 1993: 85. De Broyer and Rauschert, 1999: 286. Distribution: M Magellan Area: Chile, Seno de Reloncavi, Bahía Quillaipe, 41 ° 54 ’S 72 ° 75 ’W (sandy tidal flat) (HGA 91). Depth range: 0 m. Type-locality: Magellan Area: Chile, Seno de Reloncavi, Bahía Quillaipe, 41 ° 54 ’S 72 ° 75 ’W (sandy tidal flat) (HGA 91). Ecology: Collected from sandy tidal flat. Type material location: ZMH, Hamburg. Remarks: Since Andres (1991) described and illustrated the genus Pseudfoxiphalus, no other records or species were found.Published as part of Alonso, Gloria M., Pina, De, Rauschert, Martin & Broyer, Claude De, 2008, A catalogue of the Antarctic and sub-Antarctic Phoxocephalidae (Crustacea: Amphipoda: Gammaridea) with taxonomic, distribution and ecological data, pp. 1-40 in Zootaxa 1752 on page 27, DOI: 10.5281/zenodo.18174
Lepidepecreum urometacarinatum Andres 1983
No full textLepidepecreum urometacarinatum Andres Lepidepecreum carinatum Andres, 1983: 187, figs. 1, 2 [not L. carinatum Bate & Westwood, 1861]. Lepidepecreum urometacarinatum Andres, 1985: 134 [new name for L. carinatum Andres, 1983].–Barnard & Karaman, 1991: 496.–De Broyer & Jazdzewski, 1993: 70. Material examined. 723 specimens (males, females and juveniles), USNM 306583; 50 specimens, AM P57740; Weddell Sea, Antarctica, 74°07'S 39°38'W, 731 m, epibenthic sled, 6 February 1968, USCGC Glacier, IWSOE cruise 1, stn 0001. — 1 specimen, NMV J12923, off Enderby Land, Antarctica, Southern Ocean, 66°2.90'S 49°49.40'E to 66°3.00'S 49°49.40'E, 738 OR 806 m, epibenthic sled, M. Norman, MS Nella Dan stn HRD 012. Type locality. Antarctic Peninsula, 64°00'S 64°30'W, 100– 382 m over water depth 385 m. Remarks. These records extend the known distribution of L. urometacarinatum into the eastern Antarctic. Distribution. Antarctic Peninsula, Weddell Sea and Enderby Land, Antarctica; 100–806 m depth. ACKNOWLEDGMENTS. We thank the late Eric Dahl, who originally made the LUCE lysianassoid amphipods available to us, Gary Poore (NMV), and Rafael Lemaitre (then of SOSC) for making other material available to us; Rachael Peart and Kate Dempsey for the illustrations; and Roger Springthorpe for making the plates.Published as part of Lowry, J. K. & Stoddart, H. E., 2002, The Lysianassoid Amphipod Genera Lepidepecreoides and Lepidepecreum in Southern Waters (Crustacea: Lysianassidae: Tryphosinae), pp. 335-364 in Records of the Australian Museum 54 (3) on page 363, DOI: 10.3853/j.0067-1975.54.2002.132
INTERPRETATION OF DEPOSITIONAL FACIES AND RESERVOIR ROCK QUALITY FROM BOREHOLE, LOGS, SAN ANDRES DOLOMITE, NEW MEXICO
No full textProgram year: 1985/1986Digitized from print original stored in HDRThe Permian San Andres Formation in three cored wells in the Twin Lakes and Cato fields, New Mexico is composed of five vertically stacked tidal flat sequences. An individual tidal fiat sequence consists of evaporite (anhydrite) at the top, followed by supratidal (dolomite, anhydrite and mixtures of anhydrite and dolomite) and subtidal (dolomite or limestone) at the bottom.
The core study shows that dolomite and anhydritic dolomite are the reservoir rocks. Marine and some intertidal dolomites are the most porous and permeable. Porosity is intercrystalline with or without vugs.
Comparison of lithology, porosity, Archie porosity types in the cores with sonic, density, neutron and gamma ray borehole logs shows that lithology, vuggy porosity and tidal flat sequence may be determined from log response alone in the San Andres rocks. Vuggy porosity can be estimated from the reponses of the sonic log compared with that of the density or neutron log. Vuggy dolomites will have an Archie m (cementation exponent) value higher than 2. Calculation of water saturation will be too low and oil and gas calculations too high if the standard value of m = 2 is used in calculations in vuggy intervals
Nils Fiebig und Friederike Waldmann (Hg.): Richard M. Meyer - Germanist zwischen Goethe, Nietzsche und George. Göttingen: Wallstein, 2009
No full textAndres J. Nils Fiebig und Friederike Waldmann (Hg.): Richard M. Meyer - Germanist zwischen Goethe, Nietzsche und George. Göttingen: Wallstein, 2009. George-Jahrbuch . 01.12.2012;9 (2012/13)(1):311-313
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