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Right-brain/left-brain communication in the churchWoody, Christine Buchanan. January 2007 (has links)
Thesis (D. Min.)--Erskine Theological Seminary, 2007. / Abstract. Includes bibliographical references (leaves 145-146).
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The effect of a servant leadership seminar on church leadersBarrett, Raymond I. January 2000 (has links)
Thesis (D. Min.)--Denver Seminary, 2000. / Includes bibliographical references (leaves 227-240).
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Growing in Christ spiritual formation for church leaders at the Central Church of Christ /Seufferlein, Terry R., January 2006 (has links)
Thesis (D. Min.)--Abilene Christian University, 2006. / Abstract and vita. Includes bibliographical references (leaves 116-120).
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So old it seems new Cedar Park Assembly of God and the Cathedral Church model /Gannon, Geoffrey R. January 2005 (has links)
Thesis (M.A.)--Trinity Evangelical Divinity School, 2005. / Abstract. Includes bibliographical references (leaves 147-157).
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A study to measure pollution effects on the antithermal maintenance and diversity index of stream periphyton of Little Cedar Creek and to illustrate the succession of the diatom fractionKareyva, Albert Joseph. January 1985 (has links)
Thesis (M.S.)--Kutztown University. / Source: Masters Abstracts International, Volume: 45-06, page: 3039. Typescript. Abstract precedes thesis as preliminary leaves [1-4]. Includes bibliographical references (leaves [51-52]).
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An analysis of factors associated with compliance and dropout of sublingual immunotherapy on Japanese cedar pollinosis patients / スギ花粉症患者における舌下免疫療法の治療コンプライアンスと脱落に関する研究Imanaka, Takahiro 24 September 2019 (has links)
京都大学 / 0048 / 新制・課程博士 / 博士(医学) / 甲第22035号 / 医博第4520号 / 新制||医||1038(附属図書館) / 京都大学大学院医学研究科医学専攻 / (主査)教授 椛島 健治, 教授 佐藤 俊哉, 教授 福原 俊一 / 学位規則第4条第1項該当 / Doctor of Medical Science / Kyoto University / DFAM
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Maasai use of plants in Loliondo, Tanzania, and their impact on wild populations of two of the most used trees : Juniperus procera Endl. (Cupressaceae) and Olea africana Mill. (Oleaceae)Searle, Nicholas A. January 1999 (has links)
No description available.
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Mapping the Distribution of Atlantic White Cedar throughout southern New Jersey Using Predictive Habitat Distribution ModellingNorlin, Bryanna 27 July 2023 (has links)
No description available.
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Identifying Complex Fluvial Sandstone Reservoirs Using Core, Well Log, and 3D Seismic Data: Cretaceous Cedar Mountain and Dakota Formations, Southern Uinta Basin, Utah.Hokanson, William H. 10 March 2011 (has links) (PDF)
The Cedar Mountain and Dakota Formations are significant gas producers in the southern Uinta Basin of Utah. To date, however, predicting the stratigraphic distribution and lateral extent of potential gas-bearing channel sandstone reservoirs in these fluvial units has proven difficult due to their complex architecture, and the limited spacing of wells in the region. A new strategy to correlate the Cedar Mountain and Dakota Formations has been developed using core, well-log, and 3D seismic data. The detailed stratigraphy and sedimentology of the interval were interpreted using descriptions of a near continuous core of the Dakota Formation from the study area. The gamma-ray and density-porosity log signatures of interpreted mud-dominated overbank, coal-bearing overbank, and channel sandstone intervals from the cored well were used to identify the same lithologies in nearby wells and correlate similar stratal packages across the study area. Data from three 3D seismic surveys covering approximately 140 mi2 (225 km2) of the study area were utilized to generate spectral decomposition, waveform classification, and percent less-than-threshold attributes of the Dakota-Cedar Mountain interval. These individual attributes were combined to create a composite attribute that was merged with interpreted lithological data from the well-log correlations. The overall process resulted in a high-resolution correlation of the Dakota-Cedar Mountain interval that permitted the identification and mapping of fluvial-channel reservoir fairways and channel belts throughout the study area. In the future, the strategy employed in this study may result in improved well-success rates in the southern Uinta Basin and assist in more detailed reconstructions of the Cedar Mountain and Dakota Formation depositional systems.
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Geologic mapping of exhumed, mid-Cretaceous paleochannel complexes near Castle Dale, Emery County, Utah: On the correlative relationship between the Dakota Sandstone and the Mussentuchit Member of the Cedar Mountain FormationSorensen, Amanda Elizabeth MacKay 21 April 2011 (has links) (PDF)
Numerous well-preserved, exhumed paleochannels in the Morrison, Cedar Mountain and Dakota Sandstone formations are exposed east of Castle Dale, Utah. These channels consist primarily of point bar complexes and scattered, low sinuosity channels. To determine the vertical and lateral relationships of these channels within the Cedar Mountain and Dakota Sandstone formations, a 1:24,000 scale geologic map covering ~140 km2 was created showing the fluvial sandstones. In the study area the Cedar Mountain Formation consists, from bottom to top, of 2.5-10 m of Buckhorn Conglomerate Member equivalent units, ~80 m of the Ruby Ranch Member, and ~30 m of the Mussentuchit Member. The Dakota Sandstone consists of conglomeratic to sandy, meandering channel fills within the Mussentuchit Member. The Ruby Ranch-Mussentuchit member contact is diagnosed as the top of a laterally extensive, ~10 meter thick, maroon paleosol with calcrete horizons and root traces. When deeply weathered the contact is discernable as a shift from maroon mudstone to a pale green-white, silty mudstone. Like the balance of the Mussentuchit Member overbank deposits, the white-green mudstone is rich in smectitic clays. In the southern one-third of the mapped area, Ruby Ranch Member sandstones are thin, discontinuous channel segments surrounded by floodplain deposits. In the middle to northern area, point bar complexes dominate, some of which are laterally amalgamated. Flow direction data from four meander complexes and a low sinuosity channel indicate an average northeast flow. Dakota Sandstone channels all of which are within the Mussentuchit Member also flowed to the northeast but point bar complexes are both more numerous and more laterally continuous than in the Ruby Ranch Member, indicating deposition in an area with less accommodation space than during Ruby Ranch Member time. The data indicate the Dakota Sandstone consists exclusively of fluvial sandstones encased within the Mussentuchit Member of the Cedar Mountain Formation. Therefore, these units are coeval and simply different facies of the same depositional system. Consequently the Mussentuchit Member is considered a member facies of the Dakota Formation.
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