A Quantitative Method for Active Fault Migration Distance Assessment on both Sides of Mid‐Ocean Ridges—Based on Multi‐Beam Data-Reference-Cited by-同舟云学术

A Quantitative Method for Active Fault Migration Distance Assessment on both Sides of Mid‐Ocean Ridges—Based on Multi‐Beam Data

Published:2019-08 Issue:4 Volume:93 Page:810-819
ISSN:1000-9515
Container-title:Acta Geologica Sinica - English Edition
language:en
Short-container-title:Acta Geologica Sinica ‐ English Edition

Author:

FAN Qingkai¹²,LI Jianghai¹²,LIU Zhonglan¹³,LIU Chiheng¹²⁴

Affiliation:

1. Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education School of Earth and Space Sciences, Peking University Beijing 100871 China

2. Institute of Oil and Gas Peking University Beijing 100871 China

3. MARUM, Center for Marine Environmental Sciences University of Bremen 28334 Germany

4. Division of Geology and Mineral Resources Beijing Research Institute of Uranium Geology Beijing 100029 China

Publisher

Wiley

Subject

Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/1755-6724.13850

Reference45 articles.

1. Magmatic and tectonic extension at mid-ocean ridges: 1. Controls on fault characteristics

2. Effect of lithospheric thickness on the formation of high- and low-angle normal faults

3. Modes of faulting at mid-ocean ridges

4. Seismic structure across the rift valley of the Mid-Atlantic Ridge at 23°20′ (MARK area): Implications for crustal accretion processes at slow spreading ridges

5. Newly discovered hydrothermal fields along the ultraslow-spreading Southwest Indian Ridge around 63°E

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