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Time, space and the human community an ecological analysis of settlement in the eastern highlands of New Guinea /Pataki, Kerry Josef, January 1968 (has links)
Thesis--University of Washington, 1968. / Microfilm-xerographic reprint. Ann Arbor, Mich. : University Microfilms. Includes bibliographical references (leaves [136]-146).
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92 |
Observations on the defense mechanism in Trypanosoma equiperdum and Trypanosoma Lewisi infections in guinea-pigs and rats,Poindexter, Hildrus Augustus, January 1932 (has links)
Thesis (Ph. D.)--Columbia University, 1932. / Cover title. Vita. Description based on print version record. Bibliography: p. 19-20.
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93 |
Exploratory studies on the metabolism of warfarin in the guinea pig [Part 1] the anticoagulant action of warfarin in the guinea pig : [Part 2] The metabolism of 4-14 C-warfarin in the guinea pig /Deckert, Fred Wolfgang, January 1970 (has links)
Thesis (Ph. D.)--University of Wisconsin--Madison, 1970. / Typescript. Vita. eContent provider-neutral record in process. Description based on print version record. Includes bibliography.
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Rice in the history of the Lower Gambia-Geba areaLauer, Joseph Jerome, January 1969 (has links)
Thesis (M.A.)--University of Wisconsin--Madison, 1969. / eContent provider-neutral record in process. Description based on print version record. Includes bibliographical references.
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95 |
Studies of single neurone activity in the cochlear ganglion of the guinea pigRobertson, Donald. January 1975 (has links)
No description available.
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96 |
The acoustical impedance of the guinea-pig middle ear and the effects of the middle-ear muscles.Funnell, William Robert John. January 1972 (has links)
No description available.
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97 |
Studies on emetine cardiotoxicity in Guinea pigs /Davis, Richard Allen January 1975 (has links)
No description available.
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98 |
Functional diversity of indigenous diets in coastal Papua New Guinea : role in the nutrition transition and noncommunicable disease riskOwen, Patrick. January 2008 (has links)
No description available.
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99 |
Cultivating change : crop choices and climate in Papua New GuineaNordhagen, Stella January 2015 (has links)
No description available.
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A petrochemical study of the Mount Fubilan Intrusion and associated ore bodies, Papua New GuineaDoucette, John 02 March 2000 (has links)
The Mount Fubilan Intrusion is part of a geologically young hypabyssal stock in the Star Mountains of Papua New Guinea. This stock was mapped as the Ok Tedi Intrusive Complex and divided into four separate bodies: the Mount Fubilan, Sydney Intrusion, Kalgoorlie, and Ningi Intrusions. Hydrothermal fluids caused alteration of the Mount Fubilan, and parts of the other intrusions, to potassic and propylitic mineral assemblages and deposited gold and copper.
This investigation documents similarities and differences between the least-altered intrusive rocks of the complex and those that have undergone potassic metasomatism. The study involved detailed petrographic examination of more than two hundred thin-sections, major-oxide and trace element chemistry, and microprobe analyses of individual minerals. The magmas that crystallized to form the stock are shown to be intermediate in composition between andesite and latite. They were quartz-saturated, metaluminous, weakly iron-rich, and crystallized under oxidizing conditions. The principal mineral phases in the least-altered intrusive rocks are andesine, pyroxene, orthoclase, and quartz. The accessory mineral suite in least-altered rocks includes biotite, sphene, apatite, magnetite, and zircon.
Hornblende is present in a few samples Magmatic pyroxene is diopsidic in composition; hornblendes is cdenitic; and biotite is annitic. Potassic alteration has converted andesine to orthoclase, or mixtures of albite and orthoclase, ferro magnesian minerals to hydrothermal biotite, sphene to rutile, and magnetite to pyrite and chalcopyrite. Hydrothermal biotite is phlogopitic in composition. Gold and copper were concentrated in the zone of potassic alteration.
The mineralogical transformation of the intrusive rocks of the Mount Fubilan and associated intrusions was caused by the infiltration of hydrothermal fluids that deposited potassium, gold, and copper and that leached and removed virtually all other rock constituents. Leached components were transported away from the zone of potassic alteration and deposited in peripheral parts of the intrusive complex to form propylites, endoskarn, and massive replacement bodies or removed from the system entirely.
The Mount Fubilan intrusion was closely similar in chemistry and mineralogy to the other intrusions of the complex prior to alteration. Petrochemical differences between the Mount Fubilan Intrusion and the other intrusions were produced entirely by hydrothermal alteration. / Graduation date: 2000
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