Photomicrographs of representative mineralogy from the Nankai subduction zone (Japan)

doi:doi:10.1594/PANGAEA.969329

Photomicrographs of representative mineralogy from the Nankai subduction zone (Japan)

Photomicrographs of representative mineralogy are here presented for each unit defined in our study. Unit A is dominated by quartz and feldspar whereas clay minerals, clinopyroxene and micas are in minor proportions (S4.1 and S4.2). Quartz, especially polycrystalline quartz, is dominant within the Unit B whereas micas and clinopyroxene are low in abundance (S4.3 and S4.4). Unit C is characterized by a high content in clay minerals as well as feldspar and monocrystalline quartz (S4.5). Unit D is characterized by a high content of polycrystalline quartz (chert) and feldspar (S4.6 and S4.7).

BibTex:

@dataset{Cornard_Pauline_and_Dawson_Harriet_and_Pickering_Kevin_T_2024,
    abstract = {Photomicrographs of representative mineralogy are here presented for each unit defined in our study. Unit A is dominated by quartz and feldspar whereas clay minerals, clinopyroxene and micas are in minor proportions (S4.1 and S4.2). Quartz, especially polycrystalline quartz, is dominant within the Unit B whereas micas and clinopyroxene are low in abundance (S4.3 and S4.4). Unit C is characterized by a high content in clay minerals as well as feldspar and monocrystalline quartz (S4.5). Unit D is characterized by a high content of polycrystalline quartz (chert) and feldspar (S4.6 and S4.7).},
    author = {Cornard, Pauline and Dawson, Harriet and Pickering, Kevin T},
    doi = {10.1594/PANGAEA.969329},
    institution = {PANGAEA (Lithosphere)},
    keyword = {'deep', 'marine sediments', 'petrography analysis', 'zircon age dating'},
    title = {Photomicrographs of representative mineralogy from the Nankai subduction zone (Japan)},
    url = {https://service.tib.eu/ldmservice/vdataset/png-doi-10-1594-pangaea-969329},
    year = {2024}
}