气候变化领域集成服务门户(CCPortal): Partitioning the Ongoing Extension of the Central Apennines (Italy): Fault Slip Rates and Bulk Deformation Rates From Geodetic and Stress Data

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DOI	10.1029/2019JB018956
	Partitioning the Ongoing Extension of the Central Apennines (Italy): Fault Slip Rates and Bulk Deformation Rates From Geodetic and Stress Data
	Carafa M.M.C.; Galvani A.; Di Naccio D.; Kastelic V.; Di Lorenzo C.; Miccolis S.; Sepe V.; Pietrantonio G.; Gizzi C.; Massucci A.; Valensise G.; Bird P.
发表日期	2020
ISSN	21699313
卷号	125 期号:7
英文摘要	We investigated whether the joint inversion of geodetic and stress direction data can constrain long-term fault slip rates in the central Apennines, and ultimately how extension is partitioned among fault slip and bulk lithosphere permanent strain. Geodetic velocities are collected in the fault interseismic stage with steady secular deformation; thus, long-term estimates can be derived with a model of elastically unloading seismogenic faults within a viscously deforming lithosphere. As the average spacing of permanent Global Navigation Satellite Systems (GNSS) stations is similar to the average length of seismogenic faults (25–35 km), if not larger, we decided to merge permanent and temporary GNSS measurements, resulting in a denser geodetic data set. Given that most normal faults in the Apennines have slip rates around or below 1 mm/a, and most campaign GNSS velocities carry similar uncertainties, simple local back slip models cannot be applied. More sophisticated modeling is required to extract reasonable bulk deformation rates and long-term fault slip rates at signal-to-noise ratio of order unity. Given the spatial distribution of the GNSS network, we estimated the long-term slip rate of seven major fault systems that are in satisfactory agreement with available geological slip rates. The resulting spatial distribution of bulk deformation rates locally fits short-term transients; in other cases, they represent the currently unclear signature of tectonic processes like upper-crustal viscoplastic deformation and aseismic slip, or indicate missing faults in the adopted database. We conclude that the time is ripe for determining fault slip rates using geodetic and stress direction data, particularly where fault activity rates are hard to determine geologically. ©2020. American Geophysical Union. All Rights Reserved.
语种	英语
来源期刊	Journal of Geophysical Research: Solid Earth
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/187784
作者单位	Sezione di Sismologia e Tettonofisica, Istituto Nazionale di Geofisica e Vulcanologia, L'Aquila, Italy; Osservatorio Nazionale Terremoti, Istituto Nazionale di Geofisica e Vulcanologia, Rome, Italy; Dipartimento di Scienze della Terra e Geoambientali, Università di Bari, Bari, Italy; Sezione di Sismologia e Tettonofisica, Istituto Nazionale di Geofisica e Vulcanologia, Rome, Italy; Department of Earth, Planetary, and Space Sciences, University of California, Los Angeles, CA, United States
推荐引用方式 GB/T 7714	Carafa M.M.C.,Galvani A.,Di Naccio D.,et al. Partitioning the Ongoing Extension of the Central Apennines (Italy): Fault Slip Rates and Bulk Deformation Rates From Geodetic and Stress Data[J],2020,125(7).
APA	Carafa M.M.C..,Galvani A..,Di Naccio D..,Kastelic V..,Di Lorenzo C..,...&Bird P..(2020).Partitioning the Ongoing Extension of the Central Apennines (Italy): Fault Slip Rates and Bulk Deformation Rates From Geodetic and Stress Data.Journal of Geophysical Research: Solid Earth,125(7).
MLA	Carafa M.M.C.,et al."Partitioning the Ongoing Extension of the Central Apennines (Italy): Fault Slip Rates and Bulk Deformation Rates From Geodetic and Stress Data".Journal of Geophysical Research: Solid Earth 125.7(2020).