Paleocene-early Eocene post-subduction magmatism in Sikhote-Alin(Far East Russia):New constraints fo

来源 :地学前缘(英文版) | 被引量 : 0次 | 上传用户:aquabluesky
下载到本地 , 更方便阅读
声明 : 本文档内容版权归属内容提供方 , 如果您对本文有版权争议 , 可与客服联系进行内容授权或下架
论文部分内容阅读
New isotopic,geochemical and geochronological data justify the widespread occurrence of middle Paleocene to early Eocene (60-53 Ma) post-subduction felsic magmatism across the entire Sikhote-Alin territory (southeast-ern Russia),conform with previous observations in Northeast China,the southern Korean Peninsula,and the Inner Zone of Japan.This igneous activity in East Asia coincided with the reactivation (after tectonic quiescence between-93-60 Ma) of left-lateral strike-slip displacements along the Tan-Lu and Central Sikhote-Alin faults and with the post-60 Ma cessation of subduction/accretion recorded in the Shimanto belt of SW Japan.The Sikhote-Alin post-subduction igneous A-type rocks present diverse mineralogical and geochemical features that suggest interactions of the subducting plate with anhydrous mantle upwelling through slab tears in the continental mar-gin.The middle Paleocene-early Eocene magmatism is not related to subduction but is synchronous with strike-slip tectonics and the termination of accretionary prism development,suggesting a shift in tectonic regime from oceanic plate subduction at a convergent margin to parallel sliding and initiation of a transform continental mar-gin.These new observations are inconsistent with the current tectonic model of 60-50 Ma Izanagi-Pacific ridge subduction beneath East Asian continental margin.
其他文献
Massive gas emissions(e.g.,CO2,CH4 and SO2)during the formation of large igneous provinces(LIPs)have been suggested as the primary cause of dramatic climatic change and the consequent ecological collapses and biotic crises
选取吐鲁番新旧站2017年逐小时气温、风速对比观测资料计算小时差值并进行分级;同时选择1988—2018年逐月平均气温、风速做t检验。结果表明:(1)吐鲁番新旧站气温和风速差值均为偏态分布,多数为正且差值分布较分散,仅40.7%的气温差值在-1℃<△T<1℃之间,32.1%的气温差值在±2℃之外;46%的风速差值在-1 m·s~(-1)<△S<1 m·s~(-1)之间,21.4%的风速差值在±2
采用2002—2016年GRACE(Gravity recovery and climate experiment)重力卫星JPL-RL06M数据分析咸海流域陆地水储量变化(Terrestrial water storage change, TWSC)时空变化特征,并结合CRU TS4.03气象数据、GLDAS-Noah地表蒸散发数据和高精度土地利用数据探究气候变化与人类活动对陆地水储量的影响。结
Few global syntheses of oxygen and carbon isotope composition of pedogenic carbonates have been attempted,unlike marine carbonates.Pedogenic carbonates represen
Turbidites from the Shiquanhe-Namco Ophiolite Mélange Zone (SNMZ) record critical information about the tec-tonic affinity of the SNMZ and the evolutionary his
选取艾比湖流域降水、地表水和地下水为研究对象,结合流域水文地质资料,利用野外调查、室内试验和统计分析等方法分析了流域不同水体氢氧稳定同位素的时空变化特征。结果表明:(1)艾比湖流域降水δ~2H和δ~(18)O变化范围分别为-148.2‰~-34.5‰和-20.16‰~1.20‰,流域大气降水线斜率为6.69。降水δ~(18)O值与气温呈正相关关系,与降水量在夏季表现出显著的负相关关系。(2)地表水
利用2019年6—9月青海省干旱内陆区雨滴谱仪和雨量筒数据,运用物理检验法和统计方法,分析了超高功率集束强声波干预下近地面降雨微物理特征变化。结果表明:(1)声波干预下,累计降雨量增加,降雨量增加和减少的场次分别占研究总场次的60.87%和39.13%。平均粒径、液态水含量、雷达反射率因子、雨强和降雨动能等微物理量均值明显增大,雨强和动能增幅最为明显,分别为36.00%和69.20%。(2)声波干
Relying on the conceptual DPSIR framework and MODFLOW analysis,this study used a mixed approach to produce groundwater resource management solutions for the Najafabad area in central Iran.According to DPSIR results,agricultural activities put the highest
为深入了解石羊河上游的人工增雨效果,评估不同月份的人工增雨效果,利用统计方法对2010—2019年4—10月石羊河上游地区的人工增雨作业效果进行了检验和分析。结果表明:石羊河上游4—10月平均绝对增雨量为4.7 mm,检验结果通过0.05的显著性检验。春季(4—5月)和秋季(9—10月)人工增雨效果明显好于夏季(6—8月);4月增雨效果最好,相对增雨率在35%以上。区域历史回归分析的结果介于序列分
利用1960—2020年青藏高原东北部66个观测站日最低气温资料和NCEP/NCAR逐日再分析资料,根据百分位法确定了32个区域持续性低温事件,并对该事件发生的概率分布及影响其发生的主要环流系统进行了分析,同时探讨了冬季气候指数的极端性与低温事件发生的关联性。结果表明:(1)区域持续性低温事件主要集中在东部农业区。(2)不同类型低温事件环流差异主要表现在高层500 h Pa高度场正异常中心和负异常