Albuquerque Geology最新文献_第4页

A double-porosity model of ground-water flow in the Madera Formation based on spring hydrographs and aquifer test analyses from Placitas, New Mexico 基于春季水文曲线和新墨西哥州普莱西塔斯含水层测试分析的Madera地层地下水流动双孔隙模型

Albuquerque Geology Pub Date : 1900-01-01 DOI: 10.56577/ffc-50.393

P. Johnson

引用次数: 1

Preliminary assessment of the age of the palynoflora of the Red Tanks Member, Madera Formation, Carrizo Arroyo, New Mexico 新墨西哥州卡里佐阿罗约马德拉组红色坦克成员孢粉植物年龄的初步评估

Albuquerque Geology Pub Date : 1900-01-01 DOI: 10.56577/ffc-50.293

A. Traverse, S. Ash

引用次数: 5

Paleomagnetic and rock magnetic properties of Santa Fe Group sediments in the 98th Street core hole and correlative surface exposures, Albuquerque Basin, New Mexico 新墨西哥州阿尔伯克基盆地98街岩心孔及相关地表暴露Santa Fe组沉积物的古地磁和岩石磁性特征

Albuquerque Geology Pub Date : 1900-01-01 DOI: 10.56577/ffc-50.355

M. Hudson, John W. Marlo Mikolas, B. Allen

引用次数: 6

Topographic setting of the Rio Grande rift, New Mexico: Assessing the role of flexural "rift-flank uplift" in the Sandia Mountains 新墨西哥州里奥格兰德裂谷的地形背景:评估弯曲的“裂谷翼隆起”在桑迪亚山脉中的作用

Albuquerque Geology Pub Date : 1900-01-01 DOI: 10.56577/ffc-50.167

M. Roy, K. Karlstrom, S. Kelley, F. Pazzaglia, S. Cather

引用次数: 7

Third-day trip 2 road log, geomorphic and hydrologic response in Estancia Basin to late Pleistocene and Holocene climate change 第三天行程2路日志，Estancia盆地地貌和水文对晚更新世和全新世气候变化的响应

Albuquerque Geology Pub Date : 1900-01-01 DOI: 10.56577/ffc-50.75

R. Anderson, B. Allen

引用次数: 1

Hydrologic modeling of the Estancia Basin, New Mexico 新墨西哥州埃斯坦西亚盆地的水文模拟

Albuquerque Geology Pub Date : 1900-01-01 DOI: 10.56577/ffc-50.409

{"title":"Hydrologic modeling of the Estancia Basin, New Mexico","authors":"","doi":"10.56577/ffc-50.409","DOIUrl":"https://doi.org/10.56577/ffc-50.409","url":null,"abstract":"-A conceptual and numerical model (ESTAN97) representing the hydrologic conditions of the Estancia basin was developed based on the basin's geologic structure and available hydrologic data. Geographic information systems (GIS) techniques were used in preparing the model input files. The Estancia basin is a topo graphically closed basin in central New Mexico with an area of about 2400 mi 2· The general surface drainage and subsurface flow is toward the central part of the basin where water is discharged by evaporation from a sys tem of playas and springs. ESTAN97 was calibrated to produce predevelopment (before 1940) and historical (1940-1996) water levels and flow conditions. Water budget analysis indicated that for the period from 1940 to 1996 about 2.08 million acre-ft of water was depleted from the basin during development. About 63% of this depletion came from aquifer storage, 34% came from salvaged evaporation and 3% was captured from neigh boring basins. The historical development has resulted in water-level declines of about 60 ft at the main pump ing centers and the disruption of the Antelope and Estancia springs. Population projections were used to esti mate future growth in domestic and public water-supply uses. Future irrigation use was assumed to decrease by 5% from 1996 uses. The results indicated that aquifer storage would maintain future development for at least 40 more years. It is expected that water levels at the main pumping centers will drop an additional 60 ft by the year 2036.","PeriodicalId":429358,"journal":{"name":"Albuquerque Geology","volume":"29 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":"133827806","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: 6

Quaternary evolution of the Rio Grande near Cochiti Lake, northern Santo Domingo Basin, New Mexico 新墨西哥州圣多明各盆地北部科奇蒂湖附近的格兰德河第四纪演化

Albuquerque Geology Pub Date : 1900-01-01 DOI: 10.56577/ffc-50.371

D. Dethier

引用次数: 6

Ascent and eruption at the Albuquerque Volcanoes: A physical volcanology perspective 阿尔伯克基火山的上升和喷发:物理火山学的观点

Albuquerque Geology Pub Date : 1900-01-01 DOI: 10.56577/ffc-50.221

L. Crumpler

引用次数: 2

Correlation of Triassic strata across the Rio Grande rift, north-central New Mexico 新墨西哥州中北部里约热内卢大裂谷三叠纪地层对比

Albuquerque Geology Pub Date : 1900-01-01 DOI: 10.56577/ffc-50.305

A. Heckert

引用次数: 11

Paleoseismology of the Tijeras fault near Golden, New Mexico 新墨西哥州戈尔登附近提杰拉斯断层的古地震学

Albuquerque Geology Pub Date : 1900-01-01 DOI: 10.56577/ffc-50.201

K. Kelson, C. Hitchcock, J. Harrison

{"title":"Paleoseismology of the Tijeras fault near Golden, New Mexico","authors":"K. Kelson, C. Hitchcock, J. Harrison","doi":"10.56577/ffc-50.201","DOIUrl":"https://doi.org/10.56577/ffc-50.201","url":null,"abstract":"The 100-km-long Tijeras-Cafioncito fault system is a potential seismogenic source that extends between the Santa Fe and Albuquerque metropolitan areas of New Mexico. The fault system accommodates east-west crustal extension and provides structural linkage between the Espanola and Albuquerque basins of the active Rio Grande rift. At the Adobe Camp site northeast of Albuquerque, we conducted detailed trenching to assess the near-surface location, timing, and style of late Quaternary deformation on the southern Tijeras fault, a major component of the Tijeras-Caftoncito fault system. At Adobe Camp, the fault consists of two main strands that may represent a positive half-flower structure. The eastern fault strand is vertical and coincides with a leftdeflection in a west-flowing arroyo. The western fault strand has reverse fault geometry and dips moderately eastward; it likely merges with the eastern vertical strand in the shallow subsurface (about 30 to 40 m depth). The western strand has placed bedrock over late Quaternary deposits and coincides with northwest-facing scarps that truncate piedmont surfaces. Field relations suggest that vertical separation was produced along the western fault strand, whereas lateral offset occurred primarily on the eastern fault strand. Trench and arroyo-wall exposures show that two colluvial deposits were shed from the fault scarps along the western fault strand. The lower colluvial deposit is faulted, whereas the upper colluvium is not, thereby indicating two faulting events. The ages of these earthquakes are poorly constrained because of uncertainties in the ages of the faulted and unfaulted colluvia. However, based on the relative degree of soil development and stratigraphic position, we estimate that the colluvia most likely are late Pleistocene (11130 ka). Our interpretation is that the scarp-derived colluvia were deposited following two surface-rupturing earthquakes along the southern Tijeras fault during the late Pleistocene. If these earthquakes ruptured the entire 41-km-long southern part of the Tijeras fault, they may have been as large as moment magnitude (Mw) 7.0.","PeriodicalId":429358,"journal":{"name":"Albuquerque 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":"125390802","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: 6