"深発地震" meaning in All languages combined

See 深発地震 on Wiktionary

Noun [日本語]

Forms: しんぱつじしん
  1. 震源が深い(地下深い場所で発生する)地震。震源の深さがおおよそ60〜100kmより深い地震を指す。深さ60〜300kmの地震を「やや深発地震」、300km以深のものを「深発地震」と呼ぶ場合もある。
    Sense id: ja-深発地震-ja-noun-T0az6RNh
The following are not (yet) sense-disambiguated
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        "震源が深い(地下深い場所で発生する)地震。震源の深さがおおよそ60〜100kmより深い地震を指す。深さ60〜300kmの地震を「やや深発地震」、300km以深のものを「深発地震」と呼ぶ場合もある。"
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      "glosses": [
        "震源が深い(地下深い場所で発生する)地震。震源の深さがおおよそ60〜100kmより深い地震を指す。深さ60〜300kmの地震を「やや深発地震」、300km以深のものを「深発地震」と呼ぶ場合もある。"
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This page is a part of the kaikki.org machine-readable All languages combined dictionary. This dictionary is based on structured data extracted on 2024-10-17 from the jawiktionary dump dated 2024-10-02 using wiktextract (1fa2fea and a709d4b). The data shown on this site has been post-processed and various details (e.g., extra categories) removed, some information disambiguated, and additional data merged from other sources. See the raw data download page for the unprocessed wiktextract data.

If you use this data in academic research, please cite Tatu Ylonen: Wiktextract: Wiktionary as Machine-Readable Structured Data, Proceedings of the 13th Conference on Language Resources and Evaluation (LREC), pp. 1317-1325, Marseille, 20-25 June 2022. Linking to the relevant page(s) under https://kaikki.org would also be greatly appreciated.