Collaborative Research: Thin Crust Over the Marion Rise: Remelting the Gondwanan Mantle

合作研究：马里恩海隆上的薄地壳：冈瓦纳地幔的重熔

• 批准号: 1657826
• 负责人: Vincent Salters
• 金额: $ 16.87万
• 依托单位: Florida State University
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2018
• 资助国家: 美国
• 起止时间: 2018-10-01 至 2022-09-30
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1657826&HistoricalAwards=false
• 关键词: Collaborative; Research; Thin; Crust; Over

It has long been assumed that the Earth consists of a thin, outer, silica-rich, hardened crust overlying a thick layer of silica-poor, magnesium-rich, mantle rock known as peridotite and an inner, nickel-iron core. Compared to Earth's ~40 kilometer thick continental crust, ocean crust is generally considered to be relatively thin (i.e., 6-7 km thick). One of the most exciting discoveries in ocean sciences over the last 15 years has been the discovery that parts of the seafloor do not have normal ocean crust, but rather Earth's mantle is exposed directly on the seafloor over large regions of the Arctic, Indian, and Atlantic Oceans. Just how much of the seafloor is exposed mantle not presently known, although estimates have been made that predict up to 25%. This research comprises the US portion of a two-ship, US-German, collaborative project designed to map, collect gravity and magnetic geophysical data, and sample a large areas of the seafloor along the Southwest Indian Ridge in the western Indian Ocean to determine how much mantle rock is exposed there. Geophysical data and geochemical analysis of major and trace elements and various isotopes will be carried out post-cruise at shore-based laboratories. The results of this work, combined with ongoing French studies on the eastern portion of the southwest Indian Ridge will allow, for the first time, an accurate estimate of how much mantle is exposed along an entire mid-ocean ridge. More than 80% of this region has never been mapped and sampling has been largely restricted to a few sections of a narrow 3-mile-wide rift valley that forms the southwest Indian Ridge mid-ocean ridge spreading center. This work is important because mantle rock is very unstable at the Earth's surface, particularly on the seafloor where it is exposed to and extensively reacts with seawater. These reactions produce hydrogen and methane, which, in turn, provide energy for bacterial life in the deep sea and support what could be an extensive biomass below the seafloor that is presently not accounted for in the inventory of life supported by our planet. The reactions between seawater and mantle rock also potentially sequester carbon in the form of carbonate minerals that form by the removal of CO2 from seawater, thereby affecting global and atmospheric carbon budgets at different time scales. Broader impacts of the work include training of graduate students at three institutions, support of an early career scientist from a gender under-represented in the sciences, outreach to elementary and high schools, and public outreach. This project takes to sea a high school teacher and a scientific blogger, who will conduct live interaction sessions with students during the oceanographic expedition and who will prepare age-appropriate educational materials and radio documentaries of the research and oceanographic cruise. There is also a significant component of international collaboration with German, Italian, and Chinese scientists some of whom will participate in the expedition and interact closely with the students and US faculty, further building international relations with these scientific communities.This research consists of an oceanographic expedition to the crest of the Marion Rise on the Southwest Indian Ridge to test the hypothesis that that the Marion Rise is supported by lateral mantle heterogeneity produced by the recycling different Gondwanan mantle provinces beneath the modern ocean ridge, as opposed to a thermal anomaly due to a mantle plume. This is the first leg of a two-leg US-German-Chinese international program to study the Marion platform, a little studied part of the seafloor, and its origin. The cruise will use multibeam sonar to map the seafloor in the area, will dredge rocks for later shore-based laboratory analysis, collect gravity and magnetic geophysical data, and carry out geochemical analyses of select samples. Sea surface magnetics will be used to locate central magnetic anomalies to identify spreading centers and determine spreading rate asymmetries. Regions of a amagmatic seafloor spreading will be determined by their weak magnetic signal and lack of easily definable magnetic lineations. Gravity surveys will allow calculation of residual mantle Bouguer anomalies from which magmatically robust regions can be identified on the basis of their characteristic negative lows. In addition to on-axis work, the expedition will include extensive off-axis dredging to help delineate mantle domains and major magmatic centers. Post-cruise research includes petrographic and geochemical analysis of collected seafloor basalts and peridotites to determine the nature and origin of the mantle source in the Marion Rise area. Chinese collaborators will conduct major and trace element analyses of dredged rocks and US laboratories will analyze the isotopes and isotopic ratios of Hf, and Os as well as radiogenic isotopes of Sr, Nd, and Pb. Calculation of the mantle using geochemically determined mantle density gradients will estimate the extent of serpentinization in the exposed mantle sections. This, together with processed magnetization data, lithologic analysis of collected rock samples, and multi-channel sonar bathymetry will be used to construct a geologic map of the area to determine the tectonic evolution and crustal architecture of the Platform. This work fills a significant sampling gap on mid-ocean ridges and will enhance significantly our understanding of global mantle variability as well as provide new insights into the nature of shallow mantle convection and on the origin of mantle hotspots.This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.

长期以来，人们一直认为地球是由一个薄的、外层的、富含二氧化硅的、硬化的地壳组成的，地壳上覆盖着一层厚的、贫二氧化硅的、富含镁的地幔岩（称为橄榄岩）和一个内部的镍铁核。 与地球约40公里厚的大陆地壳相比，海洋地壳通常被认为相对较薄（即，6-7公里厚）。在过去的15年里，海洋科学中最令人兴奋的发现之一是发现部分海底没有正常的海洋地壳，而是地球的地幔直接暴露在北极，印度洋和大西洋的大部分地区的海底。究竟有多少海底是暴露的地幔目前还不知道，虽然已经作出估计，预测高达25%。这项研究包括一个由两艘船组成的美国-德国合作项目的美国部分，该项目旨在绘制地图，收集重力和磁力地球物理数据，并沿西印度洋西南印度洋海岭沿着对大面积海底进行采样，以确定那里有多少地幔岩暴露。考察后将在岸上实验室进行地球物理数据和主要元素、微量元素及各种同位素的地球化学分析。这项工作的结果，加上法国正在进行的关于西南印度洋脊东部的研究，将使人们能够第一次准确估计有多少地幔沿着整个洋中脊暴露出来。该地区80%以上的地区从未被绘制过地图，采样主要限于一个狭窄的3英里宽的裂谷的几个部分，该裂谷形成了西南印度洋脊中脊扩张中心。这项工作很重要，因为地幔岩在地球表面非常不稳定，特别是在海底，它暴露在海水中并与海水发生广泛反应。这些反应产生氢气和甲烷，而氢气和甲烷又为深海中的细菌生命提供能量，并支持海底下可能存在的大量生物量，而这些生物量目前尚未计入我们星球所支持的生命清单。 海水和地幔岩之间的反应也可能以碳酸盐矿物的形式螯合碳，这些矿物是通过从海水中去除二氧化碳而形成的，从而影响不同时间尺度上的全球和大气碳收支。这项工作的更广泛影响包括在三个机构培训研究生，支持一名来自科学界代表性不足的性别的早期职业科学家，向小学和中学推广，以及向公众推广。该项目将有一名高中教师和一名科学博客作者出海，他们将在海洋学考察期间与学生进行现场互动，并将编写适合年龄的教育材料和关于研究和海洋学考察的广播纪录片。与德国，意大利和中国科学家的国际合作也是一个重要组成部分，其中一些科学家将参加探险，并与学生和美国教师密切互动，进一步建立与这些科学界的国际关系。这项研究包括对西南印度洋海岭马里恩海隆顶部进行海洋学考察，以检验马里恩海隆是一个海洋学研究的假设。支持的横向地幔不均匀性所产生的循环不同冈瓦纳地幔省份下现代洋脊，而不是热异常，由于地幔柱。这是一个由美国、德国和中国组成的国际项目的第一站，该项目旨在研究马里恩平台，这是海底的一个小部分，以及它的起源。这次航行将使用多波束声纳绘制该地区的海底地图，挖掘岩石供以后在岸上进行实验室分析，收集重力和磁力地球物理数据，并对选定的样品进行地球化学分析。海洋表面磁学将用于定位中心磁异常，以确定扩展中心和确定扩展率不对称性。无岩浆海底扩张的区域将由其微弱的磁信号和缺乏容易确定的磁线理来确定。重力测量将允许计算剩余地幔布格异常，根据其特征负低点，可以确定岩浆活跃区域。除了轴上的工作，探险将包括广泛的离轴疏浚，以帮助划定地幔域和主要岩浆中心。航行后的研究包括对收集到的海底玄武岩和橄榄岩进行岩相学和地球化学分析，以确定马里恩海隆地区地幔源的性质和起源。中国合作者将对疏浚岩石进行主元素和微量元素分析，美国实验室将分析Hf和Os的同位素和同位素比值以及Sr，Nd和Pb的放射性同位素。利用地球化学确定的地幔密度梯度计算地幔将估计出露地幔剖面中蛇纹石化的程度。这一数据，加上经过处理的磁化数据、对收集的岩石样本进行的岩性分析和多通道声纳测深，将用于绘制该地区的地质图，以确定该平台的构造演变和地壳结构。这项工作填补了大洋中脊的一个重要的采样空白，将大大提高我们对全球地幔变化的理解，并为浅地幔对流的性质和地幔热点的起源提供新的见解。该奖项反映了NSF的法定使命，并被认为值得通过使用基金会的知识价值和更广泛的影响审查标准进行评估来支持。

项目成果

Trace Element and Isotopic Evidence for Recycled Lithosphere from Basalts from 48 to 53°E, Southwest Indian Ridge

• DOI: 10.1093/petrology/egaa068
• 发表时间: 2020-06
• 期刊: Journal of Petrology
• 影响因子: 3.9
• 作者: Jixin Wang;Huaiyang Zhou;V. Salters;H. Dick;J. Standish;Cong Wang

Mantle melting variation and refertilization beneath the Dragon Bone amagmatic segment (53°E SWIR): Major and trace element compositions of peridotites at ridge flanks

龙骨无岩浆段（53°E SWIR）下的地幔熔化变化和再肥化：山脊侧面橄榄岩的主量和微量元素组成

• DOI: 10.1016/j.lithos.2018.11.014
• 发表时间: 2019
• 期刊: Lithos
• 影响因子: 3.5
• 作者: Wang, Jixin;Zhou, Huaiyang;Salters, Vincent;Liu, Yang;Sachi-Kocher, Afi;Dick, Henry
• 通讯作者: Dick, Henry