obsic

Exceptional scientific results are OBSIC's ultimate goal. This page (below) lists citations of published results that were aided or enabled through the use of the OBSIP/OBSIC facility.
As stated in the OBSIC Instrument Use Policies and Procedures, all users of OBSIC Instrumentation are requested to cite the use and support of the OBSIC facility, by incorporating the following acknowledgement in any publications or reports resulting from the use of OBSIC instruments:
“Data used in this research were provided by instruments from the Ocean Bottom Seismic Instrument Center (https://obsic.whoi.edu), which is funded by the National Science Foundation (https://www.nsf.gov). OBSIC data are archived at the IRIS Data Management Center (http://www.iris.edu)."
Please complete the OBSIC Submit a Publication Form with any publications or reports related to your experiment.

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Filters: Author is Cai, Chen [Clear All Filters]

Journal Article

C. Cai, Wiens, D. A., Shen, W., and Eimer, M., “Water input into the Mariana subduction zone estimated from ocean-bottom seismic data”, Nature, vol. 563, pp. 389–392, 2018.

C. An, Cai, C., Zheng, Y., Meng, L., and Liu, P., “Theoretical Solution and Applications of Ocean Bottom Pressure Induced by Seismic Seafloor Motion”, Geophysical Research Letters, vol. 44, pp. 10,272–10,281, 2017.

H. Deng, An, C., Cai, C., and Ren, H., “Theoretical Solution and Applications of Ocean Bottom Pressure Induced by Seismic Waves at High Frequencies”, Geophysical Research Letters, vol. 49, p. e2021GL096952, 2022.

S. S. Wei, Wiens, D. A., van Keken, P. E., and Cai, C., “Slab temperature controls on the Tonga double seismic zone and slab mantle dehydration”, Science Advances, vol. 3, p. e1601755, 2017.

M. Eimer, Wiens, D. A., Cai, C., Lizarralde, D., and Jasperson, H., “Seismicity of the Incoming Plate and Forearc Near the Mariana Trench Recorded by Ocean Bottom Seismographs”, Geochemistry, Geophysics, Geosystems, vol. 21, p. e2020GC008953, 2020.

F. Xu, Lu, S., Cai, C., Chen, H., and Dong, S., “Constraints on the structure of the oceanic crust of the Tamu Massif by teleseismic P-wave coda autocorrelation”, Frontiers in Earth Science, vol. 11, 2023.

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