JpGU-AGU Joint Meeting 2017

講演情報

[EJ] ポスター発表

セッション記号 M (領域外・複数領域) » M-GI 地球科学一般・情報地球科学

[M-GI29] [EJ] データ駆動地球惑星科学

2017年5月20日(土) 13:45 〜 15:15 ポスター会場 (国際展示場 7ホール)

コンビーナ:桑谷 立(国立研究開発法人 海洋研究開発機構)、Kondrashov Dmitri(University of California, Los Angeles)、長尾 大道(東京大学地震研究所)、Sergey Kravtsov(University of Wisconsin Milwaukee)

[MGI29-P22] Statistical approach in the microboudin method for palaeostress analysis: reliability of the relationship between far-field differential stress and proportion of microboudinage structure of columnar grains

*松村 太郎次郎1増田 俊明2 (1.静岡大学創造科学技術大学院、2.静岡大学理学部地球科学科)

キーワード:古応力解析、数値シミュレーション、マイクロブーディン応力計、電気石、マイクロブーディン構造

The microboudinage structure of columnar mineral grains can be used as a passive marker in the palaeostress analysis of the metamorphic tectonites. In this presentation, we demonstrate the stress estimation by the numerical model that uses grain-shape data to calculate the relationship between the proportion of microboudinaged columnar grains (p) and the far-field differential stress (σ0). This model combines weakest link theory and the shear-lag model. Weakest link theory is used to derive the fracture strength of grains, whereas the shear-lag model is used to determine the relationship between the differential stress within a grain (σ) and σ0. An intact grain becomes a microboudinaged grain when σ is higher than its fracture strength at a specific point within the grain. The relationship between p and σ0 can be used to estimate the magnitude of differential stress. Here, we make calculations of p for all intact grains under increasing σ0 regardinig 50–1000 tourmaline grains shape data. These data are randomly collected from the original 1432 tourmaline grains shape data. Using the calculation result, we enable to evaluate the number of measurement grain to carry out a reasonable palaeostress analysis. This procedure will contribute to resolve the particularly time consuming when conducting stress analysis for a large number of samples within a metamorphic belt.