{"title":"新墨西哥州中南部棕榈园组中—晚始新世中间火山岩和奥列洪安山岩的U-Pb年代学","authors":"R. H. Creitz, B. Hampton, G. Mack, J. Amato","doi":"10.56577/ffc-69.147","DOIUrl":null,"url":null,"abstract":"A bstrAct —U-Pb zircon ages from the middle–late Eocene intermediate volcanic rocks of the Palm Park Formation and Orejon Andesite provide new geochronologic constraint on the duration of volcanism that took place just after the Laramide orogeny and prior to the onset of latest Eocene bimodal volcanism and initiation of the Rio Grande rift in south-central New Mexico at ~36 Ma. Presented here are nine new U-Pb zircon ages (n=247 analyses) from the Organ, Doña Ana, Robledo, and Sierra de las Uvas Mountains that fall within a range of ~45–40 Ma. The oldest age determined from this study was collected from an ash-fall tuff exposed in the lower part of the Palm Park Formation in the Robledo Mountains (Apache canyon) and yields an age of 45.0±0.7 Ma. Three samples from intermediate volcanic flows in the Orejon Andesite of the Organ Mountains (Fillmore canyon) yield ages of 44.0±1.5, 43.8±0.4, and 42.8±1.5 Ma. Four samples were collected from a series of intermediate composition (andesite to dacite) volcanic flows in the Doña Ana Mountains (Cleofas canyon) and Robledo Mountains (Faulkner canyon) and yield ages of 41.6±0.7, 41.3±0.7, and two nearly-identical ages of 41.0±0.6 Ma. The youngest age reported from this study was determined from an ash-fall tuff exposed near the top of the Palm Park Formation in the eastern part of the Sierra de las Uvas fault block and yields an age of 39.6±0.5 Ma. New data are presented here, together with previously reported ages and fossil occurrences from the Palm Park Formation, Orejon Andesite, and equivalent units throughout south-central New Mexico, including the Cleofas Andesite and Rubio Peak Formation. Based on new ages and fossil age ranges, we favor a model where these rocks were erupted and deposited over a ~10 my period between ~46–36 Ma during which mantle wedge material was re-introduced throughout south-central New Mexico just prior to onset of the Rio Grande rift.","PeriodicalId":253436,"journal":{"name":"Las Cruces Country III","volume":"152 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"3","resultStr":"{\"title\":\"U-Pb geochronology of middle�late Eocene intermediate volcanic rocks of the Palm Park Formation and Orejon Andesite in south-central New Mexico\",\"authors\":\"R. H. Creitz, B. Hampton, G. Mack, J. Amato\",\"doi\":\"10.56577/ffc-69.147\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"A bstrAct —U-Pb zircon ages from the middle–late Eocene intermediate volcanic rocks of the Palm Park Formation and Orejon Andesite provide new geochronologic constraint on the duration of volcanism that took place just after the Laramide orogeny and prior to the onset of latest Eocene bimodal volcanism and initiation of the Rio Grande rift in south-central New Mexico at ~36 Ma. Presented here are nine new U-Pb zircon ages (n=247 analyses) from the Organ, Doña Ana, Robledo, and Sierra de las Uvas Mountains that fall within a range of ~45–40 Ma. The oldest age determined from this study was collected from an ash-fall tuff exposed in the lower part of the Palm Park Formation in the Robledo Mountains (Apache canyon) and yields an age of 45.0±0.7 Ma. Three samples from intermediate volcanic flows in the Orejon Andesite of the Organ Mountains (Fillmore canyon) yield ages of 44.0±1.5, 43.8±0.4, and 42.8±1.5 Ma. Four samples were collected from a series of intermediate composition (andesite to dacite) volcanic flows in the Doña Ana Mountains (Cleofas canyon) and Robledo Mountains (Faulkner canyon) and yield ages of 41.6±0.7, 41.3±0.7, and two nearly-identical ages of 41.0±0.6 Ma. The youngest age reported from this study was determined from an ash-fall tuff exposed near the top of the Palm Park Formation in the eastern part of the Sierra de las Uvas fault block and yields an age of 39.6±0.5 Ma. New data are presented here, together with previously reported ages and fossil occurrences from the Palm Park Formation, Orejon Andesite, and equivalent units throughout south-central New Mexico, including the Cleofas Andesite and Rubio Peak Formation. Based on new ages and fossil age ranges, we favor a model where these rocks were erupted and deposited over a ~10 my period between ~46–36 Ma during which mantle wedge material was re-introduced throughout south-central New Mexico just prior to onset of the Rio Grande rift.\",\"PeriodicalId\":253436,\"journal\":{\"name\":\"Las Cruces Country III\",\"volume\":\"152 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1900-01-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"3\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Las Cruces Country III\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.56577/ffc-69.147\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Las Cruces Country III","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.56577/ffc-69.147","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 3
摘要
棕榈园组中晚始新世中期火山岩和奥列洪安山岩的锆石u - pb年龄为新墨西哥州中南部约36 Ma始新世双峰火山活动开始和里约热内卢大裂谷开始之前的火山活动持续时间提供了新的地质年代学约束。本文介绍了来自Organ, Doña Ana, Robledo和Sierra de las Uvas山脉的9个新的U-Pb锆石年龄(n=247),范围在~ 45-40 Ma之间。从这项研究中确定的最古老的年龄是在罗布莱多山脉(阿帕奇峡谷)棕榈公园组下部暴露的火山灰凝灰岩中收集的,其年龄为45.0±0.7 Ma。来自Organ山(Fillmore峡谷)Orejon安山岩的3个中间火山流样品的年龄分别为44.0±1.5、43.8±0.4和42.8±1.5 Ma。从Doña Ana山脉(Cleofas峡谷)和Robledo山脉(Faulkner峡谷)的一系列中间成分(安山岩-英安岩)火山流中采集了4个样品,产年龄分别为41.6±0.7、41.3±0.7,以及两个几乎相同的41.0±0.6 Ma。该研究报告中最年轻的年龄是在Sierra de las Uvas断块东部棕榈园组顶部附近的火山灰凝灰岩中确定的,其年龄为39.6±0.5 Ma。本文介绍了新的数据,以及先前报道的棕榈公园组、奥列洪安山岩和新墨西哥州中南部的等效单元(包括Cleofas安山岩和Rubio峰组)的年龄和化石出现情况。基于新时代和化石时代范围,我们倾向于这样一种模型:这些岩石是在~ 46-36 Ma之间的~10 Ma期间喷发和沉积的,在此期间,地幔楔物质在里约热内卢大裂谷开始之前重新引入新墨西哥州中南部。
U-Pb geochronology of middle�late Eocene intermediate volcanic rocks of the Palm Park Formation and Orejon Andesite in south-central New Mexico
A bstrAct —U-Pb zircon ages from the middle–late Eocene intermediate volcanic rocks of the Palm Park Formation and Orejon Andesite provide new geochronologic constraint on the duration of volcanism that took place just after the Laramide orogeny and prior to the onset of latest Eocene bimodal volcanism and initiation of the Rio Grande rift in south-central New Mexico at ~36 Ma. Presented here are nine new U-Pb zircon ages (n=247 analyses) from the Organ, Doña Ana, Robledo, and Sierra de las Uvas Mountains that fall within a range of ~45–40 Ma. The oldest age determined from this study was collected from an ash-fall tuff exposed in the lower part of the Palm Park Formation in the Robledo Mountains (Apache canyon) and yields an age of 45.0±0.7 Ma. Three samples from intermediate volcanic flows in the Orejon Andesite of the Organ Mountains (Fillmore canyon) yield ages of 44.0±1.5, 43.8±0.4, and 42.8±1.5 Ma. Four samples were collected from a series of intermediate composition (andesite to dacite) volcanic flows in the Doña Ana Mountains (Cleofas canyon) and Robledo Mountains (Faulkner canyon) and yield ages of 41.6±0.7, 41.3±0.7, and two nearly-identical ages of 41.0±0.6 Ma. The youngest age reported from this study was determined from an ash-fall tuff exposed near the top of the Palm Park Formation in the eastern part of the Sierra de las Uvas fault block and yields an age of 39.6±0.5 Ma. New data are presented here, together with previously reported ages and fossil occurrences from the Palm Park Formation, Orejon Andesite, and equivalent units throughout south-central New Mexico, including the Cleofas Andesite and Rubio Peak Formation. Based on new ages and fossil age ranges, we favor a model where these rocks were erupted and deposited over a ~10 my period between ~46–36 Ma during which mantle wedge material was re-introduced throughout south-central New Mexico just prior to onset of the Rio Grande rift.