GLORIA

GEOMAR Library Ocean Research Information Access

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
  • 1
    Online Resource
    Online Resource
    Elsevier BV ; 2019
    In:  Lithos Vol. 344-345 ( 2019-11), p. 464-481
    In: Lithos, Elsevier BV, Vol. 344-345 ( 2019-11), p. 464-481
    Type of Medium: Online Resource
    ISSN: 0024-4937
    RVK:
    Language: English
    Publisher: Elsevier BV
    Publication Date: 2019
    detail.hit.zdb_id: 1494884-9
    detail.hit.zdb_id: 221624-3
    SSG: 13
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 2
    Online Resource
    Online Resource
    Springer Science and Business Media LLC ; 2022
    In:  International Journal of Earth Sciences Vol. 111, No. 4 ( 2022-06), p. 1129-1148
    In: International Journal of Earth Sciences, Springer Science and Business Media LLC, Vol. 111, No. 4 ( 2022-06), p. 1129-1148
    Abstract: Maio Island (Cabo Verde Archipelago) is composed of uplifted Early Mesozoic MORB-type pillow lavas and deep-sea sediments, unconformably overlain and intruded by Miocene igneous rocks. Combined structural analyses and 40 Ar– 39 Ar dating were used to constrain the Miocene evolution of Maio. Structures and ages of uplifted Mesozoic sequences and crosscutting Miocene dykes showed that numerous intrusive events were associated with the intense growth of an igneous core complex in the middle to upper crust, causing semi-circular doming and partial disruption of the Mesozoic strata. Two nosean nephelinite dykes cut the Valanginian Batalha Formation and yielded phlogopite 40 Ar– 39 Ar ages of 10.405 ± 0.033 Ma and 10.570 ± 0.053 Ma (2σ errors). A nosean nephelinite dyke that cuts the overlying Valanginian to Early Aptian Morro Formation yielded an age of 9.273 ± 0.020 Ma. Combined with existing K–Ar and 40 Ar– 39 Ar ages, this confirmed a main period of island growth between ~ 16 and 8.7 Ma. We re-interpreted extensive polymict conglomerates, which occur below the Late Miocene Monte Penoso Formation, as landslide deposits. A nephelinite lava clast yielded a phlogopite 40 Ar– 39 Ar age of 8.666 ± 0.0274 Ma, which represents a maximum age for these landslides and thus confined a period of large-scale flank collapses and erosion to between 8.7 and 6.7 Ma. Flank collapses and further mass wasting during this period may have rejuvenated the igneous activity, i.e., resulting in the formation of the Tortonian/Messinian Monte Penoso and Malhada Pedra Formations, due to decompression-induced melting at upper mantle depths. Such interaction between flank collapses and rejuvenated volcanism may be a key to better understand ocean island evolution worldwide.
    Type of Medium: Online Resource
    ISSN: 1437-3254 , 1437-3262
    Language: English
    Publisher: Springer Science and Business Media LLC
    Publication Date: 2022
    detail.hit.zdb_id: 1477582-7
    detail.hit.zdb_id: 1477600-5
    detail.hit.zdb_id: 2075432-2
    SSG: 13
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 3
    Online Resource
    Online Resource
    Springer Science and Business Media LLC ; 2018
    In:  International Journal of Earth Sciences Vol. 107, No. 8 ( 2018-11), p. 2931-2932
    In: International Journal of Earth Sciences, Springer Science and Business Media LLC, Vol. 107, No. 8 ( 2018-11), p. 2931-2932
    Type of Medium: Online Resource
    ISSN: 1437-3254 , 1437-3262
    Language: English
    Publisher: Springer Science and Business Media LLC
    Publication Date: 2018
    detail.hit.zdb_id: 1477582-7
    detail.hit.zdb_id: 1477600-5
    detail.hit.zdb_id: 2075432-2
    SSG: 13
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...