将区域矩震级补充到GCMT:来自重建的ISC公报的观点

D. Di Giacomo, James Harris, D. Storchak
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引用次数: 0

摘要

摘要地震学家和地球科学家通常需要地震目录进行各种类型的研究。这个输入通常包含基本的地震参数,如位置(经度、纬度、深度和起源时间)以及震级信息。对于后者,矩震级Mw已成为地震学界最受追捧的震级尺度,以表征地震的大小。在这篇文章中,我们为新重建的国际地震中心公报(ISC, http://www.isc.ac.uk/)提供了有关Mw含量的信息,该公报被认为是地球地震活动的最全面记录。从中,我们从向ISC报告数据的众多机构中提取了具有Mw的震源列表。我们首先总结了全球机构(即提供全球中强地震的结果)和区域机构(即也提供特定地区小地震的结果)提供的Mw的主要时空特征。然后,我们讨论了它们的比较,不仅考虑了Mw,而且考虑了表面波震级MS和短周期体波震级mb。通过将全球质心矩张量解作为权威的全球机构,我们确定了最能补充它的区域机构,并展示了单独从全球质心矩张量获得的不同区域的频率-震级分布以及从区域机构补充的Mw。区域机构在毫瓦方面所做的工作对于提高我们对一个地区地震活动性的理解至关重要,我们呼吁在目前没有很好地覆盖这方面的地区,例如亚洲大陆和非洲的大部分地区,实施以系统方式计算毫瓦的程序。此外,还需要更多的研究来澄清全球兆瓦估算值明显高于区域兆瓦估算值的原因。在Mw与MS和mb的比较中也观察到这种差异。本文的结果来自ISC数据集存储库(http://www.isc.ac.uk/dataset_repository/)中的数据集(Di Giacomo和Harris, 2020, https://doi.org/10.31905/J2W2M64S)。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Complementing regional moment magnitudes to GCMT: a perspective from the rebuilt ISC Bulletin
Abstract. Seismologists and geoscientists in general often need earthquake catalogues for various types of research. This input usually contains basic earthquake parameters such as location (longitude, latitude, depth and origin time) as well as magnitude information. For the latter, the moment magnitude Mw has became the most sought after magnitude scale in the seismological community to characterize the size of an earthquake. In this contribution we provide an informative account of the Mw content for the newly rebuilt Bulletin of the International Seismological Centre (ISC, http://www.isc.ac.uk/), which is regarded as the most comprehensive record of the Earth's seismicity. From it, we extracted a list of hypocentres with Mw from a multitude of agencies reporting data to the ISC. We first summarize the main temporal-spatial features of the Mw provided by global agencies (i.e., providing results for moderate to great earthquakes worldwide) and regional ones (i.e., also providing results or small earthquakes in a specific area). Then we discuss their comparisons, not only by considering Mw but also the surface wave magnitude MS and short-period body wave magnitude mb. By using the Global Centroid Moment Tensor solutions as authoritative global agency, we identify regional agencies that best complement it and show examples of frequency-magnitude distributions in different areas obtained both from the Global Centroid Moment Tensor alone and complemented by Mw from regional agencies. The work done by the regional agencies in terms of Mw is fundamental to improve our understanding of the seismicity of an area and we call for the implementation of procedures to compute Mw in a systematic way in areas currently not well covered in this respect, such as vast parts of continental Asia and Africa. In addition, more studies are needed to clarify the causes of the apparent overestimation of global Mw estimations compared to regional Mw. Such difference is also observed in the comparisons of Mw with MS and mb. The results presented here are obtained from the dataset (Di Giacomo and Harris, 2020, https://doi.org/10.31905/J2W2M64S) stored at the ISC Dataset Repository (http://www.isc.ac.uk/dataset_repository/).
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