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G. Mohn

As seen in: Nature
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Articles by G. Mohn

A whole rock geochemical dataset for magmatic rocks drilled on the mid-Norwegian margin

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By P. Guo, S. Chatterjee, M. Jones, S. Planke, K. Cashman, T. Jane Takahashi, J. Millett, G. Mohn, E. C. Ferré, N. Sánchez Varela, W. W. Xu, C. Tegner, S. Lambart, H. H. Svensen, E. R. Neumann, C. E. Lesher, E. H. Cunningham, A. M. Morris, E. W. Stokke, J. Longman, C. Berndt, C. A. Alvarez Zarikian, P. Betlem, I. Y. Filina, J. Frieling, D. T. Harper, R. P. Scherer
| Nature Verified
Abstract The mid-Norwegian margin is one of the best studied volcanic rifted margins on Earth. Geophysical investigations have demonstrated the presence of well-developed inner and outer Seaward Dipping Reflectors (SDRs), landward flows, lava deltas, marginal highs, volcanic centers, ash layers, and sill complexes.
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Mode of continental breakup of marginal seas

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By G. Mohn, M. Nirrengarten
We investigated the continent-ocean transition (COT) structure of three main marginal seas in the western Pacific Ocean (South China Sea, Coral Sea, and Woodlark Basin) to determine the tectono-magmatic processes acting during continental breakup. The COT formed from the activity of a low-angle normal fault system localizing deformation during final rifting. Extension was contemporaneous with magmatic activity, including volcanic edifices, dikes, and sills in the distalmost parts of these basins.
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Rapid transition from continental breakup to igneous oceanic crust in the South China Sea

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By M. Nirrengarten, Z. Sun, H. C. Larsen, G. Mohn
| Nature Verified
H.C.L. was co-principal investigator (co-PI) for the original drilling proposal and interpretation of seismic data, co-chief scientist of expeditions 367/368, and directed the writing of the paper. G.M. is principal co-author, developed the geodynamic model jointly with H.C.L. and M.N. and was a shipboard scientist (structural geology) at expedition 368.
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