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Wiki Education Foundation-supported course assignment

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This article is or was the subject of a Wiki Education Foundation-supported course assignment. Further details are available on the course page. Student editor(s): Jalyn Buckley.

Above undated message substituted from Template:Dashboard.wikiedu.org assignment by PrimeBOT (talk) 04:24, 17 January 2022 (UTC)[reply]

Suggested Article Revisions

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  • Under "Contents," add headings for and corresponding information pertaining to "History," "Geology," and perhaps "Tectonic Activity (Earthquakes)"
  • Article needs more citations pertaining to existing facts/information, and more references regarding subject matter
  • Add a "snapshot" of information regarding the Molucca Sea Plate, including, dimensions (length, width, density), geology, location, and coordinates of the plate

Jalyn Buckley (talk) 06:10, 11 April 2018 (UTC)[reply]

Bibliography

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A. Silver, Eli & Moore, J. (1978). The Molucca Sea Collision Zone, Indonesia. Journal of Geophysical Research. 83. 1681-1691. 10.1029/JB083iB04p01681.

Bader, Anne Gaelle & Pubellier, Manuel. (2008). Forearc deformation and tectonic significance of the ultramafic Molucca Central Ridge, Talaud islands (Indonesia). Island Arc. 9. 653 - 663. 10.1111/j.1440-1738.2000.00309.x.

Fischer, TP,Hilton, DR,Sharp, ZD,Hartono, U, Clor, Laura E, Fischer, Tobias P, Hilton, David R, Sharp, Zachary D, & Hartono, Udi. (2005). Volatile and N isotope chemistry of the Molucca Sea collision zone: Tracing source components along the Sangihe Arc, Indonesia. Geochemistry, Geophysics, Geosystems G³., 6(3), N/a.

McCaffrey, R. (1991), Earthquakes and ophiolite emplacement in the Molucca Sea Collision Zone, Indonesia, Tectonics, 10(2), 433–453, doi:10.1029/90TC02553.

McCaffrey, R. , Silver, E. A. and Raitt, R. W. (2013). Crustal Structure of the Molucca Sea Collision Zone, Indonesia. In The Tectonic and Geologic Evolution of Southeast Asian Seas and Islands, D. E. Hayes (Ed.). doi:10.1029/GM023p0161

Mikhailov, V,Diament, M,Deplus, C,Louat, R, Widiwijayanti, Christina, Mikhailov, Valentin, Diament, Michel, Deplus, Christine, Louat, Rémy, . . . Gvishiani, Alexei. (2003). Structure and evolution of the Molucca Sea area: Constraints based on interpretation of a combined sea-surface and satellite gravity dataset. Earth and Planetary Science Letters, 215(1-2), 135-150.

Philippines, Iran, Alaska (and the Far North): Earthquakes 5-11 January 2017 Jennifer Young - https://www.decodedscience.org/philippines-iran-alaska-far-north-earthquakes-5-11-january-2017/60479

Pubellier, M, Bader, Anne Gaelle, & Pubellier, Manuel. (2000). Forearc deformation and tectonic significance of the ultramafic Molucca central ridge, Talaud islands (Indonesia). The Island Arc., 9(4), 653-663.

Tiberi, C,Deplus, C,Diament, M,Mikhailov, V, Widiwijayanti, Christina, Tiberi, Christel, Deplus, Christine, Diament, Michel, Mikhailov, Valentin, & Louat, Rémy. (2004). Geodynamic evolution of the northern Molucca Sea area (Eastern Indonesia) constrained by 3-D gravity field inversion. Tectonophysics, 386(3-4), 203-222.

Zhang, Q., F. Guo, L. Zhao, and Y. Wu (2017), Geodynamics of divergent double subduction: 3‐D numerical modeling of a Cenozoic example in the Molucca Sea region, Indonesia, J. Geophys. Res. Solid Earth, 122, 3977–3998, doi:10.1002/2017JB013991.

Jalyn Buckley (talk) 01:33, 28 April 2018 (UTC)[reply]

map triangle diverging slope are upside down

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Thanks for this very clear article. Got a good idea about what is happening here. One thing went wrong though, the triangles of het map show the Sangihe and Halmahera plate diving under the Molucca Sea plate (normal convention is points are toward the dipping direction), whereas the article clearly shows it is the other way around. So the triangles should be pointed the other way around. — Preceding unsigned comment added by Codiv (talkcontribs) 11:54, 6 November 2020 (UTC)[reply]

The triangles are exactly the same in original map from the source (Figure 1 in Zhang et al. 2017) that this map was taken from. Comparing it with another figure in the same paper (Figure 3) the triangles on the marked trenches show triangles on the other sides, suggesting that this is a simple map error that has been repeated in the map used in this article. Alternatively, the marked "trenches" are in this case just thrust faults. I lean towards the first explanation, but, without contacting the original paper's authors, it's hard to be certain. Mikenorton (talk) 19:47, 6 November 2020 (UTC)[reply]

Move discussion in progress

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There is a move discussion in progress on Talk:Eurasian Plate which affects this page. Please participate on that page and not in this talk page section. Thank you. —RMCD bot 23:18, 6 October 2024 (UTC)[reply]