A cost-effective three-dimensional marine controlled-source electromagnetic survey: Exploring seafloor massive sulfides

Author:

Ishizu Keiichi1ORCID,Siripunvaraporn Weerachai2ORCID,Goto Tada-nori3ORCID,Koike Katsuaki4ORCID,Kasaya Takafumi5,Iwamoto Hisanori6

Affiliation:

1. Formerly Kyoto University, Department of Urban Management, Kyoto, Japan; Tokyo Institute of Technology, Volcanic Fluid Research Center, Tokyo, Japan; and Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Research Institute for Marine Resources Utilization, Yokosuka, Kanagawa, Japan; presently University of Hyogo, Graduate School of Science, Himeji, Hyogo, Japan. (corresponding author)

2. Mahidol University, Faculty of Science, Department of Physics, Rajthewee, Bangkok, Thailand and Thailand Center of Excellence in Physics, Commission on Higher Education, Bangkok, Thailand.

3. Kyoto University, Department of Urban Management, Kyoto, Japan and University of Hyogo, Graduate School of Science, Himeji, Hyogo, Japan.

4. Kyoto University, Department of Urban Management, Kyoto, Japan.

5. Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Research Institute for Marine Resources Utilization, Yokosuka, Kanagawa, Japan.

6. Nippon Marine Enterprises, Ltd., Marine Survey Department, Kanagawa, Japan.

Abstract

A 3D marine controlled-source electromagnetic (CSEM) survey for mapping hydrocarbons uses dozens of ocean-bottom electric (OBE) receivers deployed in a grid pattern and several transmitter towlines. This study considers seafloor massive sulfides (SMS) exploration, and the horizontal survey scale of SMS is a few kilometers, which is small compared with hydrocarbon surveys of tens of kilometers. If we apply a 3D CSEM survey using a receiver deployment on grids to map SMS, high survey costs will be incurred despite the small survey size. We have developed a cost-effective 3D marine CSEM survey that uses fewer receivers than the survey with a receiver deployment on grids to reduce survey costs for SMS. This CSEM survey uses a line of OBE receivers in the center of the survey area and several transmitter towlines. Numerical tests demonstrate that our survey (seven OBE receivers) using 80% fewer receivers than the survey with a receiver deployment on grids (35 OBE receivers) is able to accurately map SMS, obtaining a performance similar to that of the receiver deployment on grids. Then, we explore SMS in the Ieyama hydrothermal area off Okinawa, southwest Japan, using our 3D CSEM survey with a line of six OBE receivers and three transmitter towlines. The resulting 3D resistivity distribution from the observed data highlights three potential SMS zones consisting of 0.2 ohm-m low resistivity embedded into 1 ohm-m sediment.

Funder

Japan Society for the Promotion of Science

Publisher

Society of Exploration Geophysicists

Subject

Geochemistry and Petrology,Geophysics

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