中国古代文言小说集《聊斋志异》外译史较长,译本众多,可是对其西班牙语译本的研究却十分鲜见,从而显得对其研究重视程度稍显不足。本文探讨了《聊斋志异》西班牙语译本的历史社会背景与译本的关系。通过对文本与副文本的分析,讨论特殊...中国古代文言小说集《聊斋志异》外译史较长,译本众多,可是对其西班牙语译本的研究却十分鲜见,从而显得对其研究重视程度稍显不足。本文探讨了《聊斋志异》西班牙语译本的历史社会背景与译本的关系。通过对文本与副文本的分析,讨论特殊历史社会背景下译者Rafael Rojas y Román对归化策略的应用。此外插图画家Joan d’Ivori也融合了中国和西方的传统神话来为此译本创造特殊的插图,可以说Rafael Rojas y Román与Joan d’Ivori共同创造了另类的中国鬼怪故事。展开更多
The San Rafael Block(SRB)is part of one of the main retroarc volcanic provinces in southern Central Andes in Mendoza,Argentina.This block is located in the Andean foothills between the orogenic front and foreland base...The San Rafael Block(SRB)is part of one of the main retroarc volcanic provinces in southern Central Andes in Mendoza,Argentina.This block is located in the Andean foothills between the orogenic front and foreland basement uplifts of late Miocene age.In order to analyze the geochronological evolution of the Quaternary volcanism in the region,several geologic and geophysical studies have been conducted.Nevertheless,the crust,where the SRB is located,has not been well characterized yet.Based on gravimetric and magnetic data,together with isostatic and elastic thickness analyses,we modeled the crustal structure of the area.Information obtained has allowed us to understand the crust where the SRB and the Payenia volcanic province are located.Bouguer anomalies indicate that the SRB presents higher densities to the North of Cerro Nevado and Moho calculations suggest depths for this block between 40 and 50 km.Determinations of elastic thickness would indicate that the crust supporting the San Rafael Block presents values of approximately 10 km,being enough to support the block loading.However,in the Payenia region,elastic thickness values are close to zero due to the regional temperature increase.展开更多
文摘中国古代文言小说集《聊斋志异》外译史较长,译本众多,可是对其西班牙语译本的研究却十分鲜见,从而显得对其研究重视程度稍显不足。本文探讨了《聊斋志异》西班牙语译本的历史社会背景与译本的关系。通过对文本与副文本的分析,讨论特殊历史社会背景下译者Rafael Rojas y Román对归化策略的应用。此外插图画家Joan d’Ivori也融合了中国和西方的传统神话来为此译本创造特殊的插图,可以说Rafael Rojas y Román与Joan d’Ivori共同创造了另类的中国鬼怪故事。
文摘The San Rafael Block(SRB)is part of one of the main retroarc volcanic provinces in southern Central Andes in Mendoza,Argentina.This block is located in the Andean foothills between the orogenic front and foreland basement uplifts of late Miocene age.In order to analyze the geochronological evolution of the Quaternary volcanism in the region,several geologic and geophysical studies have been conducted.Nevertheless,the crust,where the SRB is located,has not been well characterized yet.Based on gravimetric and magnetic data,together with isostatic and elastic thickness analyses,we modeled the crustal structure of the area.Information obtained has allowed us to understand the crust where the SRB and the Payenia volcanic province are located.Bouguer anomalies indicate that the SRB presents higher densities to the North of Cerro Nevado and Moho calculations suggest depths for this block between 40 and 50 km.Determinations of elastic thickness would indicate that the crust supporting the San Rafael Block presents values of approximately 10 km,being enough to support the block loading.However,in the Payenia region,elastic thickness values are close to zero due to the regional temperature increase.
