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”
复制标题
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
复制
发表时间:
2006
影响因子:
--
通讯作者:
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
[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