Correction to “Evidence for asymmetric nonvolcanic rifting and slow incipient oceanic accretion from seismic reflection data on the Newfoundland margin”

Correction to “Evidence for asymmetric nonvolcanic rifting and slow incipient oceanic accretion from seismic reflection data on the Newfoundland margin”
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对“纽芬兰边缘地震反射数据中不对称非火山裂谷和缓慢初期海洋增生的证据”的修正

DOI:
10.1029/2006jb004769
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发表时间:
2006
影响因子:
--
通讯作者:
G. Nunes
G. Nunes
中科院分区:
--
文献类型:
--
作者:
D. Shillington;W. Holbrook;H. Avendonk;B. Tucholke;J. Hopper;K. Louden;H. Larsen;G. Nunes

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[1]在由Donna J.Shillington,W.Steven Holbrook,Harm J.A.Van Avenonk,Brian E.Tucholke,John R.Hopper,Keith E.Louden,Hans Christian Larsen,和Gregory T.Nunes撰写的论文《来自纽芬兰边缘的地震反射数据的非对称非火山裂谷和缓慢的初始海洋沉积的证据》(Journal of GePhys ICA ICA Research,111,B09402,Do I:10.1029/2005 JB003981,2006)中,第7节的最后一句应该修改如下:[2]最后,纽芬兰边缘表观洋底内不同的外观和断层几何形状表明,在从非火山裂谷向缓慢的初始海洋增生过渡期间,存在伸展和间歇性的岩浆供应,类似于在相邻的尖岩断面上观察到的情况[Funck等,2003;Hopper等人,2004年;Lau等人,2006a,2006b]。地球物理研究杂志,第一卷。B12403,DOI:10.1029/2006JB004769,2006点击此处查看全文
[1] In the paper ‘‘Evidence for asymmetric nonvolcanic rifting and slow incipient oceanic accretion from seismic reflection data on the Newfoundland margin’’ by Donna J. Shillington, W. Steven Holbrook, Harm J. A. Van Avendonk, Brian E. Tucholke, John R. Hopper, Keith E. Louden, Hans Christian Larsen, and Gregory T. Nunes (Journal of Geophys ica l Research , 111 , B09402, do i :10 .1029/ 2005JB003981, 2006), the last sentence of section 7 should be changed as follows: [2] Finally, the variable appearance and fault geometries within apparent oceanic basement on the Newfoundland margin suggest extension and an intermittent magma supply during the transition from nonvolcanic rifting to slow incipient oceanic accretion, similar to what is observed on adjacent SCREECH transects [Funck et al., 2003; Hopper et al., 2004; Lau et al., 2006a, 2006b]. JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 111, B12403, doi:10.1029/2006JB004769, 2006 Click Here for Full Article