Tokuyama, Hidekazu; Yuasa, Makoto; Mizuno, Atsuyuki (1980): Conglomerate and sandstone petrography at DSDP Hole 58-445 [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.821290, Supplement to: Tokuyama, H et al. (1980): Conglomerate and sandstone petrography, Deep Sea Drilling Project Site 445, Philippine Sea. In: deVries Klein, G; Kobayashi, K; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 58, 629-641, https://doi.org/10.2973/dsdp.proc.58.114.1980
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Abstract:
Conglomerates and sandstones in lithologic unit V at DSDP Site 445 comprise lithic clasts, detrital minerals, bioclasts, and authigenic minerals. The lithic clasts are dominantly plagioclase-phyric basalt and microdolerite, followed by plagioclase-clinopyroxene-phyric basalt, aphyric basalt, chert, and limestone. A small amount of hornblende schist occurs. Detrital minerals are dominantly plagioclase, augite, titaniferous augite, olivine, green to pale-brown hornblende, and dark-brown hornblende, with subordinate chromian spinel, epidote, ilmenite, and magnetite, and minor amounts of diopside, enstatite, actinolite, and aegirine-augite. Bioclasts are Nummulites boninensis, Asterocyclina sp. cf. A. penuria, and some other larger foraminifers.
Correlation of cored and dredged samples indicates that the Daito Ridge is mainly composed of igneous, metamorphic, ultramafic, and sedimentary rocks. The igneous rocks are mafic (probably tholeiitic) and alkalic. The metamorphic rocks are hornblende schist, tremolite schist, and diopside-chlorite schist. The ultramafic rocks are alpinetype peridotites. Mineralogical data suggest that there were two metamorphic events in the Daito Ridge. The older one was intermediate- to high-pressure metamorphism. The younger one was contact metamorphism caused by a Paleocene volcanic event, possibly related to the beginning of spreading of the west Philippine Basin. The ultramafic rocks suffered from the same contact metamorphism.
During the Eocene, exposed volcanic and metamorphic rocks on the uplifted Daito Ridge may have supplied pebble clasts to the surrounding coast and shallow sea bottom. The steep slope offshore may have caused frequent slumping and transportation of the pebble clasts and shallow-water benthic organisms into deeper water, forming the conglomerates and sandstones treated here.
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 25.522700 * Longitude: 133.208200
Date/Time Start: 1978-01-11T00:00:00 * Date/Time End: 1978-01-11T00:00:00
Event(s):
58-445 * Latitude: 25.522700 * Longitude: 133.208200 * Date/Time: 1978-01-11T00:00:00 * Elevation: -3377.0 m * Penetration: 892 m * Recovery: 609.5 m * Location: North Pacific/BASIN * Campaign: Leg58 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 93 cores; 882.5 m cored; 0 m drilled; 69.1 % recovery
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
3 datasets
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Datasets listed in this publication series
- Tokuyama, H; Yuasa, M; Mizuno, A (1980): (Table 2) Geochemistry at DSDP Hole 58-445. https://doi.org/10.1594/PANGAEA.821288
- Tokuyama, H; Yuasa, M; Mizuno, A (1980): (Table 3) Petrography of igneous and metamorphic clasts and detrital minerals in conglomerate at DSDP Hole 58-445. https://doi.org/10.1594/PANGAEA.821289
- Tokuyama, H; Yuasa, M; Mizuno, A (1980): (Table 1) Sample descriptions at DSDP Hole 58-445. https://doi.org/10.1594/PANGAEA.821287