Geophysics

@misc{terzaghi1950mechanisms6,
    author = "Terzaghi, A. R",
    title = "Mechanisms of Landslides, in Paige, S. [C., ed., Application of Geology to Engineering Practices",
    year = "1950",
    howpublished = "New York, Geological Society of America, v. Berkey, p. 83-123; 327 pp",
    note = "talkorigins\_source = {true}; raw\_reference = {Terzaghi, A. R., 1950, Mechanisms of Landslides, in Paige, S. [C., ed., Application of Geology to Engineering Practices: New York, Geological Society of America, v. Berkey, p. 83-123; 327 pp.}"
}

@article{khachaturov1962ways,
    author = "Khachaturov, Tigran",
    title = "Ways of Improving Capital Construction and Increasing its Effectiveness",
    year = "1962",
    journal = "Problems in Economics",
    url = "https://doi.org/10.2753/pet1061-1991050323",
    doi = "10.2753/pet1061-1991050323",
    number = "3",
    openalex = "W2062624326",
    pages = "23-30",
    volume = "5"
}

@article{provotorova1963ways,
    author = "Provotorova, Valentina N.",
    title = "Ways of Improving the Effectiveness of the Lesson",
    year = "1963",
    journal = "Soviet Education",
    url = "https://doi.org/10.2753/res1060-9393050430",
    doi = "10.2753/res1060-9393050430",
    number = "4",
    openalex = "W2253934580",
    pages = "30-35",
    volume = "5"
}

@misc{gladkov1970about4,
    author = "Gladkov, V. G. and Nikitin, V. P. and Khrenov, P. M",
    title = "About the question of kinematics of halogenating in the profiles and in the folded belt of the Southern part of the Siberian Platform",
    year = "1970",
    howpublished = "Academy of Sciences of the USSR Reports, v. 190, no. 2, p. 405-408; English translation by the American Geological Institute, 1970, Academy of Science, USSR Doklady, v.190, p. 42- 45",
    note = "talkorigins\_source = {true}; raw\_reference = {Gladkov, V. G., Nikitin, V. P., and Khrenov, P. M., 1970, About the question of kinematics of halogenating in the profiles and in the folded belt of the Southern part of the Siberian Platform: Academy of Sciences of the USSR Reports, v. 190, no. 2, p. 405-408; English translation by the American Geological Institute, 1970, Academy of Science, USSR Doklady, v.190, p. 42- 45.}"
}

@misc{bazanov1977improving2,
    author = "Bazanov, E. A. and Vereshchako, I. A. and Frolov, B. M",
    title = "Improving the methods and ways to increase effectiveness of geological oil and gas reconnaissance works in Irkutsk cirque",
    year = "1977",
    howpublished = "Geology of Oil and Gas, v. 2, p. 9- 13",
    note = "talkorigins\_source = {true}; raw\_reference = {Bazanov, E. A., Vereshchako, I. A., and Frolov, B. M., 1977, Improving the methods and ways to increase effectiveness of geological oil and gas reconnaissance works in Irkutsk cirque: Geology of Oil and Gas, v. 2, p. 9- 13.}"
}

@misc{belenkiy1978ways3,
    author = "Belen'kiy, V. Y. and Kunin, N. Y",
    title = "Ways of improving the effectiveness of seismic reconnaissance when preparing [investigating] structures in Western Yakutia",
    year = "1978",
    howpublished = "Geology of Oil and Gas, v. 5, p. 22-30",
    note = "talkorigins\_source = {true}; raw\_reference = {Belen'kiy, V. Y., and Kunin, N. Y., 1978, Ways of improving the effectiveness of seismic reconnaissance when preparing [investigating] structures in Western Yakutia: Geology of Oil and Gas, v. 5, p. 22-30.}"
}

@misc{aleinikov1980dynamics1,
    author = "Aleinikov, A. L. and Bellavin, O. V. and Bulashevich, Y. P. and Tavrin, I. F. and Maksimov, E. M. and Rudkevich, M. Y. and Nalivkin, V. D. and Shablinskaya, N. V. and Surkov, V. S",
    title = "Dynamics of the Russian and West Siberian Platforms, in Bally, A. W., and et al., eds., Dynamics of Plate Interiors",
    year = "1980",
    howpublished = "Washington, D.C., American Geophysical Union and Geological Society of America, p. 53- 71",
    note = "talkorigins\_source = {true}; raw\_reference = {Aleinikov, A. L., Bellavin, O. V., Bulashevich, Y. P., Tavrin, I. F., Maksimov, E. M., Rudkevich, M. Y., Nalivkin, V. D., Shablinskaya, N. V., and Surkov, V. S., 1980, Dynamics of the Russian and West Siberian Platforms, in Bally, A. W., and et al., eds., Dynamics of Plate Interiors: Washington, D.C., American Geophysical Union and Geological Society of America, p. 53- 71.}"
}

@misc{klein1980reconnaissance,
    author = "Klein, D. and Long, C.L. and Christopherson, K.R. and Boler, F.",
    title = "Reconnaissance geophysics in the Clifton and Gillard geothermal areas, SE Arizona",
    year = "1980",
    booktitle = "Open-File Report",
    url = "https://doi.org/10.3133/ofr80325",
    doi = "10.3133/ofr80325",
    openalex = "W2155915434",
    references = "doi101029jb081i005p00801, doi10119011440571, doi10119011440911, doi1021726870401, doi103133cir726, doi103133cir790, doi103133ofr75362, doi103133ofr8096, openalexw3087408405"
}

@misc{fujita1982bibliography,
    author = "Fujita, K. and Dretzka, E.E. and Grantz, Arthur",
    title = "Bibliography of northeast Siberian geology and geophysics",
    year = "1982",
    booktitle = "Open-File Report",
    url = "https://doi.org/10.3133/ofr82616",
    doi = "10.3133/ofr82616",
    openalex = "W1534997272",
    references = "doi10100797836428741168, doi1010160040195181901311, doi101029jb081i005p00921, doi101038256015a0, doi10108000206816509474170, doi10108000206817709471081, doi10108000206817809471495, doi10108000206818209466924, doi101130001676061977881298eitbsr20co2, openalexw2970921400"
}

@article{paul1988physiological5,
    author = "Paul, G. S",
    title = "Physiological, migratorial, climatological, geophysical, survival and evolutionary implications of polar dinosaurs",
    year = "1988",
    journal = "Journal of Paleontology, v. 62, p. 640-652",
    note = "talkorigins\_source = {true}; raw\_reference = {Paul, G. S., 1988, Physiological, migratorial, climatological, geophysical, survival and evolutionary implications of polar dinosaurs: Journal of Paleontology, v. 62, p. 640-652.}"
}

@incollection{crossref2014reconnaissance,
    title = "reconnaissance geophysics",
    year = "2014",
    booktitle = "Dictionary Geotechnical Engineering/Wörterbuch GeoTechnik",
    url = "https://doi.org/10.1007/978-3-642-41714-6\_180781",
    doi = "10.1007/978-3-642-41714-6\_180781",
    openalex = "W4245370403",
    pages = "1086-1086"
}

The Mercurio structural dome is a poorly exposed and complex structure located in the transitional region between the Coahuila Calcareous Platform and the San Pedro El Gallo sector of the Sierra Madre Oriental, Mexico. It is located in the State of Chihuahua, close to the limits with Coahuila and Durango, Mexico. The dome is a circular structure, \textasciitilde 16 km in diameter, that can be seen in air-photos, satellite images, and shaded relief maps, but that has a subtle topographic expression on the ground. As seen in the field, the most conspicuous topographic features in the area are several hills with the morphology of volcanic necks that rise up to 250 m above the surrounding terrain. The deformation fringe of the dome is a series of cuesta-like low hills, less than 30 m high, where a poorly lithified volcano-sedimentary succession (litharenites, polymictic conglomerates, and ignimbrites) is almost completely masked by desert pavement, which is mainly constituted by well-rounded calcareous clasts derived from the Mesozoic sedimentary marine rocks and by less abundant Paleogene volcanic rocks exposed in the region. Inside the dome the following units are exposed: 1) the pre-volcanic basement in a NW-trending, upright, open anticline developed in limestone of the Aurora Formation, 2) a series of hills where is exposed a succession of epiclastic and volcanic rocks, which are similar, in age and lithology, to some facies of the Ahuichila Formation, and 3) a NW-trending dike, exposed at Cerro Dinamita, which is interpreted as an offshoot of the buried subvolcanic body that created the dome. The deformation fringe around the buried intrusive has a quaquaversal array in the bedding and forms a simple monocline-like structure in the NE part of the dome. A set of SE- and NW-trending plunging folds forms the SE and SW portions of the dome, respectively. The NW part of the fringe is nearly completely masked by volcanic rocks, but there is a \textasciitilde W plunging syncline in the area. Geophysical data show a broad gravimetric high in the region, and there is a distinct aeromagnetic anomaly inside the dome. The morphological expression of the dome lies just east of a NW-trending lineament of gravity and magnetic anomalies, which may be the buried portion of a normal fault shown in geologic maps of the region northwest of the studied area. Another possible cause is an alignment of buried intrusive bodies suggested by the regional aeromagnetic data, a small diorite outcrop south of Sierra El Diablo, and presence of volcanic necks in the northern portion of Sierra Los Alamos. Available geological and geophysical information was used to model a near-surface, irregular intrusive body with variable magnetic susceptibilites. This variation in susceptibilities is consistent with observed differences in rock composition in the exposed volcanic rocks and with evidence that the structure was formed by a bimodal (andesite-rhyolite) magmatic system where mixing/mingling occurred. As a whole, the set of structures is interpreted as a dome formed by forceful magma injection into a previously folded Paleogene volcano-sedimentary succession. U-Pb zircon ages were used to bracket the age of the deformation pulses registered in the rocks. Litharenites from the deformed volcano-sedimentary succession yielded an Ypresian zircon age of \textasciitilde 51 Ma. A tilted, lithic-rich ignimbrite collected near the top of the exposed volcano-sedimentary succession has mean age of 46.4 +0.8/-1.6 Ma, and the Cerro Dinamita dike has a mean age of 29.37 ± 0.24 Ma. Thus, the youngest pulse of Laramide deformation in the area is younger than \textasciitilde 46 Ma and the re-folding, associated with emplacement of the dome occurred at \textasciitilde 29 Ma. Detrital zircon U-Pb ages from Mercurio sandstones suggest dominant sediment sources from plutonic and/or volcanic rocks exposed along western Mexico. Likely subordinate sources are Mesozoic sedimentary rocks in northern and central Mexico. Distribution of detrital zircon U-Pb ages in the studied samples is similar to that documented in sandstones of the Difunta Group at the Parras and La Popa basins, except that older grains (>1.0 Ga), documented in the clastic rocks of these basins, are scarce in the sandstones of the Mercurio area.

@article{arandagómez2019reconnaissance,
    author = "Aranda Gómez, Jorge and Yutsis, Vsevolod and Juárez-Arriaga, Edgar and Ortega-Obregón, Carlos and González-Cervantes, Norma and Chávez-Cabello, Gabriel and Ramírez-Peña, César Francisco and Torres-Gaytán, David Ernesto",
    title = "Reconnaissance geology and geophysics of the Mercurio structural dome, Chihuahua, Mexico",
    year = "2019",
    journal = "Revista Mexicana de Ciencias Geológicas",
    abstract = "The Mercurio structural dome is a poorly exposed and complex structure located in the transitional region between the Coahuila Calcareous Platform and the San Pedro El Gallo sector of the Sierra Madre Oriental, Mexico. It is located in the State of Chihuahua, close to the limits with Coahuila and Durango, Mexico. The dome is a circular structure, \textasciitilde 16 km in diameter, that can be seen in air-photos, satellite images, and shaded relief maps, but that has a subtle topographic expression on the ground. As seen in the field, the most conspicuous topographic features in the area are several hills with the morphology of volcanic necks that rise up to 250 m above the surrounding terrain. The deformation fringe of the dome is a series of cuesta-like low hills, less than 30 m high, where a poorly lithified volcano-sedimentary succession (litharenites, polymictic conglomerates, and ignimbrites) is almost completely masked by desert pavement, which is mainly constituted by well-rounded calcareous clasts derived from the Mesozoic sedimentary marine rocks and by less abundant Paleogene volcanic rocks exposed in the region. Inside the dome the following units are exposed: 1) the pre-volcanic basement in a NW-trending, upright, open anticline developed in limestone of the Aurora Formation, 2) a series of hills where is exposed a succession of epiclastic and volcanic rocks, which are similar, in age and lithology, to some facies of the Ahuichila Formation, and 3) a NW-trending dike, exposed at Cerro Dinamita, which is interpreted as an offshoot of the buried subvolcanic body that created the dome. The deformation fringe around the buried intrusive has a quaquaversal array in the bedding and forms a simple monocline-like structure in the NE part of the dome. A set of SE- and NW-trending plunging folds forms the SE and SW portions of the dome, respectively. The NW part of the fringe is nearly completely masked by volcanic rocks, but there is a \textasciitilde W plunging syncline in the area. Geophysical data show a broad gravimetric high in the region, and there is a distinct aeromagnetic anomaly inside the dome. The morphological expression of the dome lies just east of a NW-trending lineament of gravity and magnetic anomalies, which may be the buried portion of a normal fault shown in geologic maps of the region northwest of the studied area. Another possible cause is an alignment of buried intrusive bodies suggested by the regional aeromagnetic data, a small diorite outcrop south of Sierra El Diablo, and presence of volcanic necks in the northern portion of Sierra Los Alamos. Available geological and geophysical information was used to model a near-surface, irregular intrusive body with variable magnetic susceptibilites. This variation in susceptibilities is consistent with observed differences in rock composition in the exposed volcanic rocks and with evidence that the structure was formed by a bimodal (andesite-rhyolite) magmatic system where mixing/mingling occurred. As a whole, the set of structures is interpreted as a dome formed by forceful magma injection into a previously folded Paleogene volcano-sedimentary succession. U-Pb zircon ages were used to bracket the age of the deformation pulses registered in the rocks. Litharenites from the deformed volcano-sedimentary succession yielded an Ypresian zircon age of \textasciitilde 51 Ma. A tilted, lithic-rich ignimbrite collected near the top of the exposed volcano-sedimentary succession has mean age of 46.4 +0.8/-1.6 Ma, and the Cerro Dinamita dike has a mean age of 29.37 ± 0.24 Ma. Thus, the youngest pulse of Laramide deformation in the area is younger than \textasciitilde 46 Ma and the re-folding, associated with emplacement of the dome occurred at \textasciitilde 29 Ma. Detrital zircon U-Pb ages from Mercurio sandstones suggest dominant sediment sources from plutonic and/or volcanic rocks exposed along western Mexico. Likely subordinate sources are Mesozoic sedimentary rocks in northern and central Mexico. Distribution of detrital zircon U-Pb ages in the studied samples is similar to that documented in sandstones of the Difunta Group at the Parras and La Popa basins, except that older grains (>1.0 Ga), documented in the clastic rocks of these basins, are scarce in the sandstones of the Mercurio area.",
    url = "https://doi.org/10.22201/cgeo.20072902e.2019.3.1340",
    doi = "10.22201/cgeo.20072902e.2019.3.1340",
    number = "3",
    openalex = "W2993860291",
    pages = "357-377",
    volume = "36",
    references = "doi1010160926985194900221, doi101016jepsl200909013, doi101016jgsf201511006, doi101016s0009254101003552, doi101038142234b0, doi101139e83094, doi10119011438369, doi1018814epiiugs2013v36i3002, doi1021130530027, doi1021130530469"
}

@article{monto2019improving,
    author = "Monto, Arnold S and Petrie, Joshua G",
    title = "Improving Influenza Vaccine Effectiveness: Ways to Begin Solving the Problem",
    year = "2019",
    journal = "Clinical Infectious Diseases",
    url = "https://doi.org/10.1093/cid/ciz416",
    doi = "10.1093/cid/ciz416",
    number = "10",
    openalex = "W2944972328",
    pages = "1824-1826",
    volume = "69",
    references = "doi101016jcell201803030, doi101016jvaccine201302053, doi101016s147330991170295x, doi101086595861, doi101093cidcis574, doi101093cidcit736, doi101093infdisjiy103, doi101126science1097211, doi1015585mmwrmm6706a2, openalexw4292433366"
}

adaptation does not occur during production of this cell-based vaccine. The development of this now entirely mammalian-based vaccine system, which incorporates both hemagglutinin and neuraminidase, ensures that the significant protective antigens are equivalent to the strains recommended by the World Health Organization (WHO) in both amino acid sequence and glycosylation pattern. The inclusion of both proteins in a vaccine may provide an advantage over recombinant vaccines containing hemagglutinin alone. Findings from real world effectiveness studies support the use of cell-based influenza vaccines.

@article{doi103390vaccines11010052,
    author = "Rockman, Steven and Laurie, Karen and Ong, Chi Wi and Rajaram, Sankarasubramanian and McGovern, Ian and Tran, Vy Anh and Youhanna, John",
    title = "Cell-Based Manufacturing Technology Increases Antigenic Match of Influenza Vaccine and Results in Improved Effectiveness",
    year = "2022",
    journal = "Vaccines",
    abstract = "adaptation does not occur during production of this cell-based vaccine. The development of this now entirely mammalian-based vaccine system, which incorporates both hemagglutinin and neuraminidase, ensures that the significant protective antigens are equivalent to the strains recommended by the World Health Organization (WHO) in both amino acid sequence and glycosylation pattern. The inclusion of both proteins in a vaccine may provide an advantage over recombinant vaccines containing hemagglutinin alone. Findings from real world effectiveness studies support the use of cell-based influenza vaccines.",
    url = "https://doi.org/10.3390/vaccines11010052",
    doi = "10.3390/vaccines11010052",
    openalex = "W4312202403",
    references = "doi101093cidciaa1944, doi101093ofidofac532"
}

@inproceedings{malsagova2022neurodidactic,
    author = "Malsagova, Maryam and Lezina, Valeriya and Ivanov, Pavel",
    title = "NEURODIDACTIC WAYS OF IMPROVING THE EFFECTIVENESS OF ADULT EDUCATION",
    year = "2022",
    booktitle = "NEUROSCIENCE FOR MEDICINE AND PSYCHOLOGY",
    url = "https://doi.org/10.29003/m2836.sudak.ns2022-18/221",
    doi = "10.29003/m2836.sudak.ns2022-18/221",
    openalex = "W4293273953",
    pages = "221-221"
}