Analysis of Circum-Antarctic Ocean Basin Paleobathymetry and Structure

环南极洋盆古水深及结构分析

• 批准号: 9418936
• 负责人: Dennis Hayes
• 金额: $ 19.2万
• 依托单位: Columbia University
• 依托单位国家: 美国
• 项目类别: Continuing Grant
• 财政年份: 1995
• 资助国家: 美国
• 起止时间: 1995-03-15 至 2000-02-29
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=9418936&HistoricalAwards=false
• 关键词: Analysis; Circum; Antarctic; Ocean; Basin

Abstract This award supports two principal investigations that utilize the recently completed Antarctic Marine Geological and Geophysical synthesis and the associated digital bathymetric, sediment thickness, and crustal structure data files. These, used along with published digital crustal age data and spreading rate data for the circum-polar region will allow development of paleographic reconstructions, complete with paleobathymetry for a variety of geologic times from the mid-Cretaceous to the present. The crustal age and spreading rate data files are needed both to unload the sediments and reposition the depths to account for the effects of accrued crustal subsidence due to cooling and isostasy. An important benefit of determining the most plausible paleobathymetry will be to arm circulation and climate modellers with constraints necessary to refine their models and to further evaluate the sensitivity of such models to submarine morphological barriers and changing basin sizes. The second proposed application of the digital age and spreading rate files is to test hypotheses that selected oceanic crustal parameters of layer velocities and thicknesses, as well as small-scale seafloor roughness, are age and/or spreading rate dependent. Establishing such relationships is likely to lead to new discoveries about the underlying casual processes effecting crustal evolution. The Southern Ocean Marine Geological and Geophysical Atlas and other digital data provide an excellent opportunity to test such hypotheses for a significantly large fraction of the World Ocean.

该奖项支持利用最近完成的南极海洋地质和地球物理综合以及相关的数字水深、沉积物厚度和地壳结构数据文件进行的两项主要调查。这些数据与已公布的数字地壳年龄数据和环极地区的扩张速度数据一起使用，将有助于开发古地理重建，并完成从白垩纪中期到现在的各种地质时代的古地形测量。需要地壳年龄和扩展速率数据文件来卸载沉积物和重新定位深度，以考虑由于冷却和均衡而累积的地壳下沉的影响。确定最合理的古生物测量学的一个重要好处将是为环流和气候模型建模者提供必要的约束，以完善他们的模型，并进一步评估这种模型对海底形态障碍和不断变化的盆地大小的敏感性。数字年龄和扩张率档案的第二个拟议应用是检验以下假设，即选定的洋壳层速度和厚度参数以及小规模海底粗糙度取决于年龄和(或)扩张率。建立这样的关系可能会导致对影响地壳演化的潜在偶然过程的新发现。南大洋海洋地质和地球物理地图集和其他数字数据为检验世界大洋相当大一部分的这种假设提供了极好的机会。