Collaborative Research: Neoproterozoic Rifting of Utah: Geochronology, Tectonics, Sequence Stratigraphy

对于罗迪尼亚的断裂和与之相关的西劳伦西亚裂谷史，人们提出了各种各样的板块重建理论，但模型仍然存在争议。为了解决这个问题，来自爱达荷州立大学、犹他州立大学和韦伯州立大学的一个研究小组正在调查犹他州和爱达荷州南部的新元古代（11亿至5.42亿年前）沉积物，以测试裂谷形成和发展的不同模型：1)大约7.5亿年前，与岩浆柱的初始爆发有关的持久裂谷；2) 7.2亿~ 6.7亿年前的大陆分离；或3)寒武纪初期（约5.4亿年前）裂谷的形成。该团队将对新元古代地层、地层、构造、锆石物源和地质年代学进行综合研究。具体方法包括：对关键剖面进行详细的层序地层学、沉积学和岩石学研究；伴生火山岩地球化学微量元素分析确定构造-岩浆环境；利用激光烧蚀-多集电极-电感耦合等离子体质谱法、高分辨率离子探针和热离子体质谱法对原生火山锆石和碎屑锆石进行U-Pb定年；玄武岩流中角闪石的Ar-Ar定年锆石Hf同位素分析区域沉降史模拟。碎屑锆石种群的U-Pb测年和Hf同位素分析将有助于揭示源区和古地理，最年轻的火山锆石年龄为最大沉积年龄提供了重要的支撑。新元古代标志着地球历史上一些最深刻的地质变化，包括罗迪尼亚超大陆的分裂、极端的气候变化和快速的生物多样化。对于罗迪尼亚的断裂和与之相关的西劳伦西亚裂谷史，人们提出了各种各样的板块重建理论，但模型仍然存在争议。解决这一争议的重要证据存在于犹他州和爱达荷州东南部的新元古代地层中。这些地层构成了Laurentia和随后的科迪勒拉造山带的裂谷西缘的一个关键但不完全了解的部分。这项研究项目将在理解这些地层的历史方面取得重要进展，并导致对美国西部早期构造发展的不同模式的区分。

Various plate reconstructions have been proposed for break up of Rodinia and for the associated rifting history of western Laurentia, but models remain controversial. To address this problem, a research team from Idaho State University, Utah State University, and Weber State University is investigating Neoproterozoic (between 1,100 and 542 million years ago) deposits in Utah and southern Idaho in order to test different models for rift initiation and development: 1) protracted rifting at approximately 750 million years ago associated with an initial breakout of a magmatic plume; 2) continental separation between 720 and 670 million years ago; or 3) rift initiation near the beginning of the Cambrian (about 540 million years ago). The team will employ an integrated field, stratigraphic, structural, zircon provenance, and geochronologic study of Neoproterozoic strata. Specific approaches include: detailed sequence stratigraphic, sedimentologic, and petrologic studies of critical sections; geochemical trace-element analysis of associated volcanic rocks to determine tectono-magmatic setting; U-Pb dating of primary volcanic and detrital zircons using a combination of laser ablation-multicollector-inductively coupled plasma mass spectrometry, sensitive high-resolution ion microprobe, and thermal ion mass spectrometry methods; Ar-Ar dating of hornblende from basalt flows; Hf isotopic analysis of zircons; and modeling of regional subsidence histories. U-Pb dating and Hf isotopic analysis of detrital zircon populations will shed light on source areas and paleogeography, with ages of youngest reworked volcanic zircons providing important brackets for maximum depositional ages.The Neoproterozoic marks some of the most profound geologic changes in Earth history, including break up of the supercontinent Rodinia, extreme climate changes, and rapid biologic diversification. Various plate reconstructions have been proposed for break up of Rodinia and for the associated rifting history of western Laurentia, but models remain controversial. Evidence important for the resolution of this controversy lies in the Neoproterozoic strata of Utah and southeastern Idaho. These strata form a critical, but incompletely understood part of the rifted western margin of Laurentia and subsequent Cordilleran orogenic belt. This research project will make important strides in understanding the history of these beds and lead to discrimination between opposing models for the early tectonic development of the western United States.