Sm–Nd isotopic geochemistry of Precambrian to Paleozoic granitoid suites and the deep-crustal structure of the southeast margin of the Newfoundland Appalachians
Sm–Nd isotopic geochemistry of Precambrian to Paleozoic granitoid suites and the deep-crustal structure of the southeast margin of the Newfoundland Appalachians
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DOI：
10.1139/e95-019
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发表时间：
1995-02
影响因子：
1.4
通讯作者：
A. Kerr;G. Jenner;B. Fryer
中科院分区：
文献类型：
--
作者：
A. Kerr;G. Jenner;B. Fryer
在纽芬兰阿巴拉契亚山脉的中东部移动的带，晚前寒武纪基底内层的eNd值为-3到+2，但寒武-奥陶纪变质沉积岩的初始eNd值低于-7。
In the Eastern Central Mobile Belt of the Newfoundland Appalachians, late Precambrian basement inliers have eNd from −3 to +2, but Cambro-Ordovician metasedimentary rocks have initial eNd below −7....