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The Chinese Wax Mine: A Unique Oil-Impregnated Rock Deposit 中国的蜡矿:一种独特的石油浸渍岩矿床
Utah Geology Pub Date : 1900-01-01 DOI: 10.34191/ug-2-1_79
H. Ritzma
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引用次数: 1
Earthquake Epicenters in Utah July-December 1974 1974年7月至12月犹他州地震震中
Utah Geology Pub Date : 1900-01-01 DOI: 10.34191/ug-2-2_135
K. Cook
{"title":"Earthquake Epicenters in Utah July-December 1974","authors":"K. Cook","doi":"10.34191/ug-2-2_135","DOIUrl":"https://doi.org/10.34191/ug-2-2_135","url":null,"abstract":"The general earthquake epicenters in and near Utah for July through December 1974, with dates of occurrences and approximate Richter magnitudes, are listed","PeriodicalId":398645,"journal":{"name":"Utah Geology","volume":"26 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"122579876","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Classification of Ripple Marks 纹痕的分类
Utah Geology Pub Date : 1900-01-01 DOI: 10.34191/ug-3-2_85
L. R. High, M. Picard
{"title":"Classification of Ripple Marks","authors":"L. R. High, M. Picard","doi":"10.34191/ug-3-2_85","DOIUrl":"https://doi.org/10.34191/ug-3-2_85","url":null,"abstract":"Although ripple marks are extensively used in paleogeographic and environmental reconstructions, there is no generally accepted classification of them. The few formal classifications that have been proposed and the many informal classifications that have been used commonly recognize two major classes of ripples: current and either wave or oscillation types. Despite the seeming simplicity of this system, confusion has arisen because usage varies considerably. In some cases the same ripple type has been called current, wave-formed, or oscillation ripples by different authors. To resolve this problem we propose a classification that recognizes four major ripple types: wave formed, current formed, interference, and eolian. Three of the groups are aqueous, the fourth eolian. Within each group several varieties are distinguished. The most common varieties are: (wave-formed) oscillation, linear, and wave-dominated combined-flow; (current-formed) cuspate, linguoid, dune, antidune, and current-dominated combined-flow; (interference) tadpole nest, ladderback, cuspate and secondary, and rhomboid; and (eolian) sand ripples. Common names are retained, even where past usage is ambiguous, because they are descriptive and already in general use. Each ripple variety is readily identified by descriptive criteria that are related to mode of formation. Thus the classification is both genetic and descriptive. Accordingly, the ripple types can be identified objectively and also are useful for environmental reconstructions.","PeriodicalId":398645,"journal":{"name":"Utah Geology","volume":"27 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"134373416","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Wind Tides of the Great Salt Lake 大盐湖的风潮
Utah Geology Pub Date : 1900-01-01 DOI: 10.34191/ug-5-1_17
A. Lin, Po Wang
{"title":"Wind Tides of the Great Salt Lake","authors":"A. Lin, Po Wang","doi":"10.34191/ug-5-1_17","DOIUrl":"https://doi.org/10.34191/ug-5-1_17","url":null,"abstract":"Essential features of hydrographic and meteorological characteristics of wind tides on Great Salt Lake are described. Three major modes of seiching are found; and the fundamental mode has a period of 6.13 hours. The implications of these forces on the geomorphology of the lake are also discussed.","PeriodicalId":398645,"journal":{"name":"Utah Geology","volume":"24 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"134428922","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 2
Largest Known Landslide of Its Type in the United States- A Failure by Lateral Spreading in Davis County, Utah 美国已知最大的同类型滑坡-犹他州戴维斯县横向扩散的失败
Utah Geology Pub Date : 1900-01-01 DOI: 10.34191/ug-2-1_83
Richard L Van Horn
{"title":"Largest Known Landslide of Its Type in the United States- A Failure by Lateral Spreading in Davis County, Utah","authors":"Richard L Van Horn","doi":"10.34191/ug-2-1_83","DOIUrl":"https://doi.org/10.34191/ug-2-1_83","url":null,"abstract":"","PeriodicalId":398645,"journal":{"name":"Utah Geology","volume":"57 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"114495026","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 3
Kaibab Limestone and Associated Strata, Circle Cliffs , Utah 凯巴布石灰岩及伴生地层，犹他州圆崖
Utah Geology Pub Date : 1900-01-01 DOI: 10.34191/ug-1-1_5
W. A. Girdley
{"title":"Kaibab Limestone and Associated Strata, Circle Cliffs , Utah","authors":"W. A. Girdley","doi":"10.34191/ug-1-1_5","DOIUrl":"https://doi.org/10.34191/ug-1-1_5","url":null,"abstract":"Exposed Permian rocks studied in the Circle Oiffs region are the upper part of the White Rim Sandstone Formation of the Cutler Group and the overlying Kaibab Limestone. The former is composed of calcareous and dolomitic sandstones and sandy dolomites formed under stable tectonic conditions in a nearshore marine environment by reworking of the underlying aeolian portion of the White Rim Member. The Kaibab Limestone is actually a slightly calcareous, partly sandy, glauconitic dolomite which was chiefly a biomicrite before dolomitization. It formed in shallow, though quiet, marine waters under tectonically quiescent conditions. It disconformably overlies the White Rim Sandstone. Detrital intertidal and very shallow subtidal sediments of the lowermost Moenkopi Formation (Triassic), mostly chert breccias, overlie the irregular, partly channeled surface of the Kaibab Limestone. This ' attests to post-Kaibab emergence and erosion. Uniformity of lithologies and thicknesses of individual Permian beds traced across the Circle Cliffs Anticline demonstrate the absence of a late Permian paleostructure.","PeriodicalId":398645,"journal":{"name":"Utah Geology","volume":"16 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"121384768","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Structural Geology and Petroleum Potential of the South Flank of the Uinta Mountain Uplift, Northeastern Utah 犹他州东北部尤塔山隆起南侧构造地质与油气潜力
Utah Geology Pub Date : 1900-01-01 DOI: 10.34191/ug-2-2_129
J. Campbell
{"title":"Structural Geology and Petroleum Potential of the South Flank of the Uinta Mountain Uplift, Northeastern Utah","authors":"J. Campbell","doi":"10.34191/ug-2-2_129","DOIUrl":"https://doi.org/10.34191/ug-2-2_129","url":null,"abstract":"The transition between the Uinta basin and the Uinta uplift is masked by Tertiary and Quaternary sediments, so that both the position and the structural style of the boundary are unclear. Seismic data and recently drilled wells help to clarify the character of the boundary as having upthrust geometry, which is typical of the Rocky Mountain foreland. The structural configuration thus interpreted is significant to petroleum entrapment in a zone paralleling the entire south flank of the Uinta Mountains.","PeriodicalId":398645,"journal":{"name":"Utah Geology","volume":"143 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"124561165","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 1
Summary of Stratigraphy in the Mineral Range, Beaver and Millard Counties, Utah 犹他州比弗县和米勒德县矿物范围地层学综述
Utah Geology Pub Date : 1900-01-01 DOI: 10.34191/ri-84
C. Petersen
{"title":"Summary of Stratigraphy in the Mineral Range, Beaver and Millard Counties, Utah","authors":"C. Petersen","doi":"10.34191/ri-84","DOIUrl":"https://doi.org/10.34191/ri-84","url":null,"abstract":"Many persons are presently interested in the geology of the Mineral Range because lands having potential for geothermal resources are nearby. This paper has been prepared to make available unpublished stratigraphic data dealing directly with the Mineral Range, and also to apply current stratigraphic nomenclature from nearby areas to the Mineral Range. It is apparent from the following text that problems still exist with stratigraphy of the Mineral Range and additional field work should be done.","PeriodicalId":398645,"journal":{"name":"Utah Geology","volume":"67 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"127220436","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Gold Springs Mining District, Iron County, Utah, and Lincoln County, Nevada 金泉矿区，铁县，犹他州和林肯县，内华达州
Utah Geology Pub Date : 1900-01-01 DOI: 10.34191/ug-3-1_23
Lee I. Perry
{"title":"Gold Springs Mining District, Iron County, Utah, and Lincoln County, Nevada","authors":"Lee I. Perry","doi":"10.34191/ug-3-1_23","DOIUrl":"https://doi.org/10.34191/ug-3-1_23","url":null,"abstract":"Gold and silver mineralization in the Gold Springs mining district on the Utah-Nevada border is restricted to veins in Tertiary volcanic rocks. Mining began in 1897 and continued intermittently until the early 1940's. The principal mines have been the Jennie, Little Buck, Snowflake, Independence, Aetna, and Jumbo. Three mines had mills where ores were beneficiated. However, these mills were primitive and met with varying success. Few records were kept; nevertheless the district is credited with producing 9,335 ounces of gold, 40,279 ounces of silver, 12,031 pounds of copper, and 19,268 pounds of lead. The past production and this study of the surface and the underground workings indicate that the ore deposits are small but high in grade.","PeriodicalId":398645,"journal":{"name":"Utah Geology","volume":"10 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"126095780","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Small Channel-Fill Sequences in the Duchesne River Formation Near Vernal, Utah: Possible Examples of Transitions from Meandering to Braided Stream Deposits 犹他州Vernal附近Duchesne河组的小河道充填层序:曲流河沉积向辫状河沉积过渡的可能例子
Utah Geology Pub Date : 1900-01-01 DOI: 10.34191/ug-3-1_61
T. Maxwell, M. Picard
{"title":"Small Channel-Fill Sequences in the Duchesne River Formation Near Vernal, Utah: Possible Examples of Transitions from Meandering to Braided Stream Deposits","authors":"T. Maxwell, M. Picard","doi":"10.34191/ug-3-1_61","DOIUrl":"https://doi.org/10.34191/ug-3-1_61","url":null,"abstract":"Small channel-fill sequences in the Duchesne River Formation (Eocene-Oligocene?) are especially well exposed between Roosevelt and Vernal, Utah, where they consist of discrete sandstone lenses set in silty claystone. Thicknesses of the channel deposits range from 5 to 10 meters. Widths are in tens of meters.","PeriodicalId":398645,"journal":{"name":"Utah Geology","volume":"31 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"121497589","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
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