Jansen, Max N., MacLeod, Christopher J. ORCID: https://orcid.org/0000-0002-0460-1626, Lissenberg, C. Johan ORCID: https://orcid.org/0000-0001-7774-2297, Parkinson, Ian J. and Condon, Daniel J.
2024.
Relationship between of D-MORB and E-MORB magmatism during crustal accretion at mid-ocean ridges: evidence from the Masirah ophiolite (Oman).
Geochemistry, Geophysics, Geosystems
25
(3)
, e2023GC011361.
10.1029/2023GC011361
|
|
|
Jansen, Maximiliaan
2023.
Exposed ocean crust on Masirah Island, SE Oman:
Crustal accretion and melt evolution at an ancient slow-spreading mid-ocean ridge.
PhD Thesis,
Cardiff University.
Item availability restricted. |
|
|
| de Graaff, Sietze J., Percival, Lawrence M.E., Kaskes, Pim, Déhais, Thomas, de Winter, Niels J., Jansen, Max N., Smit, Jan, Sinnesael, Matthias, Vellekoop, Johan, Sato, Honami, Ishikawa, Akira, Spassov, Simo, Claeys, Philippe and Goderis, Steven 2022. Geochemical records of the end-Triassic Crisis preserved in a deep marine section of the Budva Basin, Dinarides, Montenegro. Palaeogeography, Palaeoclimatology, Palaeoecology 606 , 111250. 10.1016/j.palaeo.2022.111250 |
|
|
| Klaver, Martijn, Luu, Tu-Han, Lewis, Jamie, Jansen, Maximiliaan N., Anand, Mahesh, Schwieters, Johannes and Elliott, Tim 2021. The Ca isotope composition of mare basalts as a probe into the heterogeneous lunar mantle. Earth and Planetary Science Letters 570 , 117079. 10.1016/j.epsl.2021.117079 |
|
|
Graaff, S. J., Goodenough, K. M., Klaver, M., Lissenberg, C. J. ORCID: https://orcid.org/0000-0001-7774-2297, Jansen, M. N., Millar, I. and Davies, G. R.
2019.
Evidence for a moist to wet source transition throughout the Oman-UAE ophiolite, and implications for the geodynamic history.
Geochemistry, Geophysics, Geosystems
20
(2)
, pp. 651-672.
10.1029/2018GC007923
|
|
|
Jansen, M. N., Lissenberg, C. J. ORCID: https://orcid.org/0000-0001-7774-2297, Klaver, M., de Graaff, S. J., Koornneef, J. M., Smeets, R. J., MacLeod, C. J. ORCID: https://orcid.org/0000-0002-0460-1626 and Davies, G. R.
2018.
Isotopic variation in Semail Ophiolite lower crust reveals crustal-level melt aggregation.
Geochemical Perspectives Letters
8
, pp. 37-42.
10.7185/geochemlet.1827
|
|
|



Up a level