Collaborative Research: Diffusion of Helium in Calcite

合作研究：方解石中氦的扩散

• 批准号: 0609752
• 负责人: E. Bruce Watson
• 金额: --
• 依托单位: Rensselaer Polytechnic Institute
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2006
• 资助国家: 美国
• 起止时间: 2006-07-01 至 2008-06-30
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0609752&HistoricalAwards=false
• 关键词: Collaborative; Research; Diffusion; Helium; Calcite

Isotope thermochronology is an important tool in a variety of geologic studies including, in particular, investigations of uplift-erosion-deformation and basin heating. With a few exceptions, these studies have been focused on minerals with relatively high concentrations of either K or U. In this project, the investigators will study the diffusion of He in the low-U mineral calcite to better understand the potential for the use of calcite as a (U+Th)/He thermochronometer. Although typical marine calcites have [U]5ppm, problems associated with this low concentration can be overcome by increasing sample size and in many rocks (i.e., limestones and marbles) calcite crystals greater than 1 mm in diameter are common. Preliminary investigations on the diffusivity of He in igneous, metamorphic, and sedimentary calcite indicate a closure temperature for He of ~65C for a cooling rate of 10C/m.y. These extremely promising preliminary results will be confirmed by additional analyses and by comparing lab-induced diffusion with diffusive histories in nature, and calcite versus dolomite diffusion. The ultimate purpose of this research is to determine the temperature at which He is retained in calcite. This work has great potential because calcite is an essential mineral in both limestones and marbles and these rocks contain no other mineral which can be used to determine time-temperature history. The applications in which this technique might be used include analysis of the history of sedimentary basins (the temperature of sedimentary basins is an important consideration in the search for petroleum), the uplift of mountain belts, and speleology.

同位素热年代学是各种地质研究的重要工具，特别是隆起-侵蚀-变形和盆地加热的研究。除了少数例外，这些研究都集中在K或U浓度相对较高的矿物上。在这个项目中，研究人员将研究He在低铀矿物方解石中的扩散，以更好地了解方解石作为（U+Th）/He热时计的潜力。虽然典型的海洋方解石的[U]为5 ppm，但与这种低浓度相关的问题可以通过增加样品尺寸来克服，并且在许多岩石中（即，石灰石和大理石）直径大于1毫米的方解石晶体是常见的。对He在火成岩、变质方解石和沉积方解石中扩散率的初步研究表明，He在10 ℃/m. y的冷却速率下的闭合温度为~ 65 ℃。这些非常有前途的初步结果将证实额外的分析和比较实验室诱导的扩散与扩散历史的性质，方解石与白云石扩散。本研究的最终目的是确定He保留在方解石中的温度。这项工作有很大的潜力，因为方解石是石灰岩和大理石中的基本矿物，这些岩石不含其他矿物，可用于确定时间-温度历史。这种技术可能被用于的应用包括分析沉积盆地的历史（沉积盆地的温度是寻找石油的重要考虑因素），山脉带的隆起和洞穴学。