Izu-Bonin-Mariana Rear Arc - The missing half of the subduction factory, 30 March – 30 May 2014

التفاصيل البيبلوغرافية
العنوان: Izu-Bonin-Mariana Rear Arc - The missing half of the subduction factory, 30 March – 30 May 2014
المؤلفون: Tamura, Y., Barker, A. K., Busby, C. J., Berger, J. L. R., Blum, P., Bongiolo, E. M., Guèrin, G., Bordiga, M., Andrews, G. D. M., DeBari, S. M., Gill, J. B., Kars, M. A. C., Hamelin, C., Kita, Z. A., Jia, Jihui, Konrad, K., John, E. H., Mahony, S. H., Jonas, A.-S., Martini, M., Jutzeler, M., Miyazaki, T., Musgrave, R. J., Schindlbeck, J. C., Nascimento, N. B., Schmitt, A. K., Nichols, A. R. L., Straub, S. M., Ribeiro, J. M., Vautravers, M. J., Sato, T., Yang, Yang
سنة النشر: 2014
المجموعة: OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel)
الوصف: International Ocean Discovery Program (IODP) Hole U1436A (proposed Site IBM-4GT) lies in the western part of the Izu fore-arc basin, ~60 km east of the arc-front volcano Aogashima, ~170 km west of the axis of the Izu-Bonin Trench, 1.5 km west of Ocean Drilling Program (ODP) Site 792, and at 1776 meters below sea level (mbsl). It was drilled as a 150 m deep geotechnical test hole for potential future deep drilling (5500 meters below seafloor [mbsf]) at proposed Site IBM-4 using the D/V Chikyu. Core from Site U1436 yielded a rich record of Late Pleistocene explosive volcanism, including distinctive black glassy mafic ash layers that may record large-volume eruptions on the Izu arc front. Because of the importance of this discovery, Site U1436 was drilled in three additional holes (U1436B, U1436C, and U1436D), as part of a contingency operation, in an attempt to get better recovery on the black glassy mafic ash layers and enclosing sediments and to better constrain the thickness of the mafic ash layers. IODP Site U1437 is located in the Izu rear arc, ~330 km west of the axis of the Izu-Bonin Trench and ~90 km west of the arc-front volcanoes Myojinsho and Myojin Knoll, at 2117 mbsl. The primary scientific objective for Site U1437 was to characterize “the missing half of the subduction factory”; this was because numerous ODP/Integrated Ocean Drilling Program sites had been drilled in the arc to fore-arc region (i.e., ODP Site 782A Leg 126), but this was the first site to be drilled in the rear part of the Izu arc. A complete view of the arc system is needed to understand the formation of oceanic arc crust and its evolution into continental crust. Site U1437 on the rear arc had excellent core recovery in Holes U1437B and U1437D, and we succeeded in hanging the longest casing ever in the history of R/V JOIDES Resolution scientific drilling (1085.6 m) in Hole U1437E and cored to 1806.5 mbsf. The stratigraphy at Site U1437 was divided into seven lithostratigraphic units (I–VII) that were distinguished from each other ...
نوع الوثيقة: report
وصف الملف: text
اللغة: English
Relation: https://oceanrep.geomar.de/id/eprint/25748/1/350PR.pdf; Tamura, Y., Barker, A. K., Busby, C. J., Berger, J. L. R., Blum, P., Bongiolo, E. M., Guèrin, G., Bordiga, M., Andrews, G. D. M., DeBari, S. M., Gill, J. B., Kars, M. A. C., Hamelin, C., Kita, Z. A., Jia, J., Konrad, K., John, E. H., Mahony, S. H., Jonas, A. S., Martini, M., Jutzeler, M., Miyazaki, T., Musgrave, R. J., Schindlbeck, J. C. , Nascimento, N. B., Schmitt, A. K., Nichols, A. R. L., Straub, S. M., Ribeiro, J. M., Vautravers, M. J., Sato, T. and Yang, Y. and IODP Expedition 350 (2014) Izu-Bonin-Mariana Rear Arc - The missing half of the subduction factory, 30 March – 30 May 2014. Open Access . IODP Preliminary Report, 350 . UNSPECIFIED, 172 pp. DOI 10.14379/iodp.pr.350.2014 .
DOI: 10.14379/iodp.pr.350.2014
الاتاحة: https://oceanrep.geomar.de/id/eprint/25748/
https://oceanrep.geomar.de/id/eprint/25748/1/350PR.pdf
https://doi.org/10.14379/iodp.pr.350.2014
Rights: info:eu-repo/semantics/openAccess
رقم الانضمام: edsbas.7AF3EB82
قاعدة البيانات: BASE
الوصف
DOI:10.14379/iodp.pr.350.2014