nkysdb: なかよし論文データベース
増本 広和 様の 共著関連データベース
+(A list of literatures under single or joint authorship with "増本 広和")
共著回数と共著者名 (a list of the joint author(s))
発行年とタイトル (Title and year of the issue(s))
2013: 南海トラフ巨大分岐断層の掘削コア試料における鉱物組成および炭質物分析(SSS31 13)
Analyses of mineral composition and carbonaceous material in the megasplay fault of the Nankai Trough (SSS31 13)
2014: 化石巨大分岐断層における高温流体発生の痕跡とその空間的分布(SSS30 33)
Generation of high temperature fluid and its spatial distribution in an ancient megasplay fault (SSS30 33)
2014: 南海トラフ巨大分岐断層の暗灰色ガウジ資料における摩擦発熱履歴の再検討(SSS32 P01)
Re evaluation of frictional heat recorded in the dark gouge of a megasplay fault at the Nankai Trough (SSS32 P01)
2014: 巨大分岐断層深部 浅部における摩擦発熱レベル 炭質物のラマン分光からの推定 (SSS30 15)
Levels of frictional heat along deep to shallow parts of the megasplay fault: a Raman spectroscopic analyses of CM (SSS30 15)
2015: 南海トラフ巨大分岐断層の暗灰色ガウジにおけるイライト化反応の定量的評価(R13 O 10)
Quantitative analysis of illitization in a dark gouge along the megasplay fault in the Nankai Trough (R13 O 10)
2016: 南海トラフ巨大分岐断層における断層運動によって促進されたイライト化反応(SSS02 P16)
Faulting promoted illitization along the megasplay fault in the Nankai Trough (SSS02 P16)
2016: 曹長石のメカノケミカル粉砕による表面ラジカルの生成とその定量(SCG60 06)
The behavior of surface radicals on mechanochemically activated silicates (SCG60 06)
2017: 付加体における断層の摩擦発熱指標としての粘土鉱物の熱分解反応(R14 P 4)
Thermal decomposition of kaolinite and chlorite as a proxy for earthquake slip along an imbricate thrust fault in an accretionary prism (R14 P 4)
2018: 粘土鉱物の熱分解反応からみたプレート境界断層の熱履歴とすべり挙動(R14 P 6)
Dehydroxylation kinetics of clay minerals and its application to friction heating along an imbricate thrust in an accretionary prism (R14 P 6)
2019: 粘土鉱物の熱分解反応からみた付加体中のimbricate衝上断層のすべり挙動(SSS14 08)
Dehydroxylation kinetics of clay minerals and its application to friction heating along an imbricate thrust in an accretionary prism (SSS14 08)
2022: 窒素ガス吸着法を用いた沈み込み帯断層の微小間隙構造分析
Micro pore structural analysis of subduction zone faults using nitrogen gas adsorption method
2024: 沈み込み帯浅部断層の膨潤作用(SCG46 P20)
Seismic fault slip variation caused by smectite swelling in shallow subduction zones (SCG46 P20)