首页> 外文OA文献 >The IAB Iron-Meteorite Complex: A Group, Five Subgroups, Numerous Grouplets, Closely Related, Mainly Formed by Crystal Segregation in Rapidly Cooling Melts
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The IAB Iron-Meteorite Complex: A Group, Five Subgroups, Numerous Grouplets, Closely Related, Mainly Formed by Crystal Segregation in Rapidly Cooling Melts

机译:IAB铁陨石复合体:一组,五个子组,密切相关的许多小组,主要由快速冷却的熔体中的晶体偏析形成

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摘要

We present new data or iron meteorites that are members of group IAB or are closely related to this large group, and we have also reevaluated some of our earlier data for these irons. In the past it was not possible to distinguish IAB and IIICD irons on the basis of their positions on element-Ni diagrams. We now find that plotting, the new and revised data yields six sets of compact fields on element-Au diagrams, each set corresponding to a compositional group. The largest set includes the majority (approximately equal to 70) of irons previously designated IA: We christened this set the IAB main group. The remaining five sets we designate subgroups within the IAB complex. Three of these subgroups have Au contents similar to the main group, and form parallel trends in most element-Ni diagrams. The groups originally designated IIIC and IIID are two of these subgroups: they are now well resolved from each other and from the main group. The other low-Au subgroup has Ni contents just above the main group. Two other IAB subgroups have appreciably higher Au contents than the main group and show weaker compositional links to it. We have named these five subgroups on the basis of their Au and Ni contents. The three subgroups having Au contents similar to the main group are the low-Au (L) subgroups the two others the high-Au (H) subgroups. The Ni contents are designated high (H), medium (M), or low (L). Thus the old group IIID is now the sLH subgroup. the old group IIIC is the sLM subgroup. In addition, eight irons assigned to two grouplets plot between sLL and sLM on most element-Au diagrams. A large number (27) of related irons plot outside these compact fields but nonetheless appear to be sufficiently related to also be included in the IAB complex.
机译:我们提供了属于IAB组或与该大组有密切关系的新数据或铁陨石,并且我们还重新评估了这些铁的一些早期数据。过去,不可能根据元素镍图上的位置来区分IAB和IIICD铁。现在我们发现,绘制新数据和修改后的数据会在元素Au图上产生六组紧凑字段,每组对应于一个组成组。最大的组包括以前指定为IA的大部分铁(大约等于70):我们将其命名为IAB主组。剩下的五组将指定IAB复合体内的子组。这些子组中的三个具有与主要组相似的Au含量,并且在大多数元素Ni图中形成平行趋势。最初指定为IIIC和IIID的小组是这些子小组中的两个:现在彼此和主要小组都得到了很好的解决。另一个低Au子组的Ni含量正好位于主要组的正上方。 IAB的其他两个亚组的Au含量明显高于主要亚组,并且与其之间的组成联系较弱。我们根据金和镍的含量命名了这五个亚组。具有与主要组相似的Au含量的三个子组是低Au(L)子组,另外两个是高Au(H)子组。 Ni含量被指定为高(H),中(M)或低(L)。因此,旧的IIID组现在是sLH子组。旧的IIIC组是sLM子组。此外,在大多数元素-Au图上,分配给两个小组的八个铁杆在sLL和sLM之间绘制。大量(27)的相关铁标绘在这些致密区域之外,但看起来也足够相关,也包含在IAB复合物中。

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