# Anderson, Thomas F. 1970-

Overview
Works: 34 works in 55 publications in 1 language and 845 library holdings Criticism, interpretation, etc  Guidebooks  Conference proceedings  Pictorial works PQ7389.P49, 868.6409
Publication Timeline
1970 | |2020
Key
Publications by Thomas F Anderson
Most widely held works by Thomas F Anderson
Everything in its place : the life and works of Virgilio Piñera by Thomas F Anderson( Book )
6 editions published in 2006 in English and held by 305 libraries worldwide
"Everything in Its Place: The Life and Works of Virgilio Pinera is a seminal book that fills a major gap in Cuban and Latin American literary criticism. In addition to being the most comprehensive study to date of the life and work of Virgilio Pinera, this is the first book in English on this major twentieth-century Cuban author. In this study Thomas F. Anderson draws extensively on unpublished manuscripts and diverse critical writings, bringing new insights into how Pinera's works responded to key literary influences as well as events in his life and in Cuban political and cultural history."--BOOK JACKET
Carnival and national identity in the poetry of Afrocubanismo by Thomas F Anderson( Book )
3 editions published in 2011 in English and Undetermined and held by 223 libraries worldwide
The poetry associated with Afrocubanismo has been of great interest to academics since the movement began in the late 1920s. Thomas Anderson's detailed analysis infuses new life into the study of these remarkable works. Focusing on the representations of carnival and its comparsas (carnival bands and music), it offers new readings of poems by seminal Cuban poets, demonstrating how their writings on and about these traditions both contributed to and detracted from the development of a recognizable Afro-Cuban identity
Stable isotopes in sedimentary geology ( Book )
3 editions published in 1983 in English and held by 200 libraries worldwide
The trials of a country editor an original sketch by Thomas F Anderson( Book )
7 editions published in 1889 in English and held by 62 libraries worldwide
Stable isotopes in sedimentary geology SEPM short course no. 10, Dallas 1983 ( Book )
1 edition published in 1983 in English and held by 6 libraries worldwide
Stable isotope variations in coals and associated mineral matter by Thomas F Anderson( Book )
1 edition published in 1983 in English and held by 5 libraries worldwide
Jack Schultz : May 7, 1904-April 29, 1971 by Thomas F Anderson( Book )
1 edition published in 1975 in English and held by 5 libraries worldwide
Physical Techniques in biological research ( Book )
2 editions published in 1966 in English and held by 3 libraries worldwide
PHYSICAL, CHEMICAL, AND BIOPHYSICAL CHARACTERIZATION OF VIRUSES AND VIRUS SYSTEMS ( Book )
3 editions published between 1952 and 1955 in English and held by 3 libraries worldwide
Nova Scotia, the land of Evangeline and the tourist's paradise reached in 15 to 17 hours by the Yarmouth SteamShip Co. (Limited) by Thomas F Anderson( Book )
1 edition published in 1893 in English and held by 3 libraries worldwide
Corporeal sustenance and degradation : ailing bodies in the works of Virgilio Piñera by Thomas F Anderson( Book )
2 editions published in 1998 in English and held by 2 libraries worldwide
Source of saline groundwater in basal Pennsylvanian sandstones, southwestern Illinois : implicatons for fluid mixing and water-rock interactions by Hue-Hwa Hwang( Computer File )
1 edition published in 1996 in English and held by 1 library worldwide
Saline groundwater is common in basal Pennsylvanian sandstones in southwestern Illinois. It is an environmental concern because well water is an important source of drinking water for local residents and farms. The origin of this saline groundwater is poorly understood. In this study, I combine hydrochemistry, isotope geochemistry, and petrography to evaluate the importance of fluid mixing and water-rock interactions in producing the saline groundwater
The politics of consumption and excretion in Reinaldo Arenas's 'Termina el desfile' by Thomas F Anderson( Article )
1 edition published in 2002 in English and held by 1 library worldwide
Cells and tissues. By T.F. Anderson [and others]. 2nd ed. Ed. A.W. Pollister by Thomas F Anderson( Book )
1 edition published in 1966 in English and held by 1 library worldwide
Mineralogy and isotopic composition of sulfur in ODP Hole 118-735B gabbros, supplementary data to: Alt, Jeffrey C; Anderson, Thomas F (1991): Mineralogy and isotopic composition of sulfur in layer 3 gabbros from the Indian Ocean, Hole 735B. In: Von Herzen, RP; Robinson, PT; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 118, 113-125 by Jeffrey C Alt( Computer File )
in English and held by 1 library worldwide
Sulfide mineralogy, sulfur contents, and sulfur isotopic compositions were determined for samples from the 500-m gabbroic section of Ocean Drilling Program Hole 735B in the southwest Indian Ocean. Igneous sulfides (pyrrhotite, chalcopyrite, pentlandite, and troilite) formed by accumulation of immiscible sulfide droplets and crystallization from intercumulus liquids. Primary sulfur contents average around 600 ppm, with a mean sulfide d34S value near 0 per mil, similar to the isotopic composition of sulfur in mid-ocean ridge basalt glass. Rocks from a 48-m interval of oxide gabbros have much higher sulfur contents (1090-2530 ppm S) due to the increased solubility of sulfur in Fe-rich melts. Rocks that were locally affected by early dynamothermal metamorphism (e.g., the upper 40 m of the core) have lost sulfur, averaging only 90 ppm S. Samples from the upper 200 m of the core, which underwent subsequent hydrothermal alteration, also lost sulfur and contain an average of 300 ppm S. Monosulfide minerals in some of the latter have elevated d34S values (up to +6.9 per mil), suggesting local incorporation of seawater-derived sulfur. Secondary sulfides (pyrrhotite, chalcopyrite, pentlandite, troilite, and pyrite) are ubiquitous in trace amounts throughout the core, particularly in altered olivine and in green amphibole. Pyrite also locally replaces igneous pyrrhotite. Rocks containing secondary pyrite associated with late low-temperature smectitic alteration have low d34S values for pyrite sulfur (to - 16.6 per mil). These low values are attributed to isotopic fractionation produced during partial oxidation of igneous sulfides by cold seawater. The rocks contain small amounts of soluble sulfate (6% of total S), which is composed of variable proportions of seawater sulfate and oxidized igneous sulfur. The ultimate effect of secondary processes on layer 3 gabbros is a loss of sulfur to hydrothermal fluids, with little or no net change in d34S
Nova Scotia, the land of Evangeline and the tourist's paradise : reached in 15 to 17 hours by the Yarmouth Steamship Co. (Limited) by Thomas F Anderson( Book )
1 edition published in 1892 in Undetermined and held by 1 library worldwide
A stable isotope study on the origin of permineralized peat zones in the Herin Coal by Thomas F Anderson( Book )
1 edition published in 1980 in English and held by 1 library worldwide
Mechanisms of dolomitization in seawater and origin of the Middle Ordovician dolomites in the Illinois Basin by Wanbing Li( Computer File )
1 edition published in 1994 in English and held by 1 library worldwide
This investigation focuses on the chemistry of dolomitization and the geochemical and petrographic characteristics of the Middle Ordovician limestones and dolostones in the Illinois basin. The often cited dolomitization equation:$$\rm CaCO\sb3 + Mg\sp{2+} = CaMg(CO\sb3)\sb2 + Ca\sp{2+}$$cannot be applied to dolomite formation in seawater, because in seawater both calcite and dolomite are supersaturated. However, seawater (as a marine pore fluid) has the ability to dolomitize calcite and aragonite. In seawater, crystallization of calcite, aragonite, and dolomite drives the fluid from a region of calcite saturation to a region of calcite undersaturation, resulting in dolomitization. Seawater is a better dolomitizing fluid than a seawater-fresh water mixing-zone fluid from thermodynamic, kinetic and mass-balance considerations. The rate of dolomitization increases with increasing salinity, which is reflected in the fact that dolomite commonly occurs in hypersaline marine environments. I hypothesize the existence of dolomite domains in magnesian calcite, and propose a "dolomite-domain" model to explain the microscopic process for dolomitization of magnesian calcite. Dolomitization occurs along domain boundaries, where calcite is dissolved while dolomite precipitates as overgrowth on dolomite domains. This model can explain the preservation of fabrics and geochemical signatures during dolomitization of magnesian calcite. The wide variety of Middle Ordovician dolomites in the Illinois basin provides an opportunity to apply the above theoretical considerations. Both the Everton and Joachim Formations contain extensive dolomites that are associated with evaporite minerals and have other supratidal features. Those dolomites were formed in hypersaline environments during deposition and early diagenesis. The dolomites of Platteville and Galena Groups are not associated with evaporites and supratidal features. Nevertheless, petrographic observations, geochemical data, and theoretical consideration suggest that they also were mostly formed during deposition and early diagenesis in normal marine to hypersaline environments which are closely associated with the Wisconsin Arch. Later diagenesis by meteoric fluids and/or basinal brines might have altered oxygen isotopic composition of the dolomites. Hydrothermal fluids which had migrated through the granitic basement might have been responsible for the high $\sp{87}$Sr/$\sp{86}$Sr and low $\delta\sp{18}$O values of some dolomites in northern Illinois as well as for the source of metals in nearby Mississippi Valley Type (MVT) ore deposits. These conclusions are supported by geochemical simulations
Stable isotopes in sedimentary geology : Dallas, 1983 ( Book )
1 edition published in 1983 in English and held by 1 library worldwide

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