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论莫尔特曼的创造进化论:一个圣灵论的视角

宗教学研究 2024年第3期 155-160页

作者：李聪陈家富山东大学犹太教与跨宗教研究中心山东大学哲学与社会发展学院

莫尔特曼就创造论与进化论之间的冲突提出了独特的观点。他认为两者并非截然对立的理论,而是存在互补关系。创造论与进化论的冲突在于其意识形态化,莫尔特曼指出,解决冲突的方法在于构建进化的诠释学理论,把创造论和进化论放在彼此的情... 详细信息

莫尔特曼就创造论与进化论之间的冲突提出了独特的观点。他认为两者并非截然对立的理论,而是存在互补关系。创造论与进化论的冲突在于其意识形态化,莫尔特曼指出,解决冲突的方法在于构建进化的诠释学理论,把创造论和进化论放在彼此的情境中作出互相的诠释。他从三位一体的创造论出发,提出了一种圣灵论的解释,即圣灵就是世界进化的能量,为进化提供方向,并引导世界向着共同体而进化。

关键词：莫尔特曼创造论意识形态化圣灵进化论三位一体互补关系截然对立

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新能源船舶永磁同步电机无位置传感器控制的研究

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船电技术 2024年第3期44卷 27-31页

作者：杨泽贤陈嘉福武汉长海高新技术有限公司武汉430233

为了实现新能源船舶永磁同步电机(Permanent Magnet Synchronous Motor,简称PMSM)全速域无位置传感器控制,本文采用低速I/f控制结合中高速模型参考自适应观测器的全速域无位置传感器复合控制算法。该方法实现了新能源船舶推进无位置传... 详细信息

为了实现新能源船舶永磁同步电机(Permanent Magnet Synchronous Motor,简称PMSM)全速域无位置传感器控制,本文采用低速I/f控制结合中高速模型参考自适应观测器的全速域无位置传感器复合控制算法。该方法实现了新能源船舶推进无位置传感器控制系统的平稳可靠运行,在新能源船舶电力推进中具有较强的实际意义。

关键词：新能源船舶 PMSM 无位置传感器 I/f控制模型参考自适应

Late Carboniferous Vertical Crustal Growth in Northern North China Craton: Evidence from Zircon U-Pb Age and Depleted Hf Isotope of the Dongwanzi Syenite

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Acta Geologica Sinica(English Edition) 2020年第1期94卷 206-207页

作者： MA Xu chen Bin chen jiafu Key Laboratory of Ministry of Education on Safe Mining of Deep Metal Mines Department of GeologyNortheastern UniversityShenyang 110004China Department of Earth and Space Sciences Southern University of Science and TechnologyShenzhen 518055China

Objective Though the Central Asian Orogenic Belt (CAOB) is characterized by widespread Phanerozoic crustal growth,there is little juvenile crust documented in its southeastern segment,northern margin of the North China Craton(NCC)(Zhang et al,2007,2009).Late Carboniferous Dongwanzi ultramafic-mafic cumulate complex occurs in northern margin of the NCC and is intruded by a syenite with depleted Sr-Nd isotopes (Ma et al.,2014).However,the age and petrogenesis of this syenite is poorly *** this study,we present new petrological,zircon U-Pb and Hf isotopic data of the Dongwanzi syenite,in order to put insights on its formation age and petrogenetic relationship with cumulates.

关键词： Evidence from Zircon U-Pb Age and Depleted Hf Isotope of the Dongwanzi Syenite Northern Late Carboniferous Vertical Crustal Growth in Northern North China Craton

Identity and Differences Between Chinese and Western Cultural Philosophy

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学术界 2018年第11期 262-272页

作者： chen jiafu Wang Weili College English Teaching and Research Department Tianjin Agricultural University

Cultural philosophy refers to the study of cultural principles with philosophical viewpoints and methods to form a theoretical system of cultural views and cultural *** mainly discusses the history and development of culture,the motive force and conditions of culture,the role of tradition in social history,the comparison of various cultures,and the conflict and blending of *** paper attempts to explore an effective way to integrate the two modes of thinking of Chinese and Western cultural philosophy through a comparative analysis of the differences and identity between Chinese and Western cultural *** study of cultural identity and differences between China and Western countries has a certain practical significance for cross-cultural communication in China.

关键词： cultural philosophy differences identity

Detrital Zircon U-Pb Geochronology and Provenance of the Hebukesaier Formation in the Shaerbuerti Mountains,Northern West Junggar:Implication for Devonian Subduction of the Junggar–Balkhash Ocean

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Acta Geologica Sinica(English Edition) 2020年第5期94卷 1410-1427页

作者： LIANG Hao chen jiafu MA Xu YANG Hongzhang XIN Mingyang Department of Geology Northeastern UniversityShenyang 110819China Department of Earth Planetaryand Space SciencesUniversity of CaliforniaLos Angeles90095USA

Limited Devonian magmatic record in northern West Junggar leads to contrasting models on its tectonic *** this study,we conducted LA-ICP-MS U-Pb dating on detrital zircons of two sandstones from the Hebukesaier Formation in the Shaerbuerti *** zircons with oscillatory zoning are characterized by high Th/U(>0.3)and low La/Yb(<0.15),indicating their magmatic *** youngest zircon ages of two samples are 402±2 Ma and 406±2 Ma,respectively,suggesting that the Hebukesaier Formation was deposited at the Early *** zircon age patterns show single peaks(at ca.424 Ma,n=157),which indicates that these clastics were likely proximal accumulation after short distance *** of the Hebukesaier Formation was the Xiemisitai and Shaerbuerti *** zircon ages range from 481 Ma to 395 Ma,which indicates that there was relatively continuous Early Paleozoic magmatism in the Xiemisitai and Shaerbuerti Mountains since the Early *** spectrums of sampled detrital zircons are distinct from those of Lower Devonian strata either in southern West Junggar or in East Junggar,which implies for individual tectonic evolution of northern West *** favor that Lower Devonian Hebukesaier Formation was developed in a fore–arc setting due to the northward subduction of the Junggar–Balkhash Ocean.

关键词： geochronology detrital zircon fore-arc Devonian West Junggar

Petrogenesis and Tectonic Implications of Middle Ordovician Ocean Island Basalts from the Chagantaolegai Ophiolitic Mélange in Junggar,NW China

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Acta Geologica Sinica(English Edition) 2021年第4期95卷 1099-1111页

作者： chen jiafu LI Rongyan MA Haitao HAN Baofu LIU Junlai Key Laboratory of Ministry of Education on Safe Mining of Deep Metal Mines Department of GeologyNortheastern UniversityShenyang 110819China Department of Earth Planetaryand Space SciencesUniversity of CaliforniaLos Angeles 90095USA Ministry of Education Key Laboratory of Orogenic Belts and Crustal Evolution School of Earth and Space SciencesPeking UniversityBeijing 100871China State Key Laboratory of Geological Process and Mineral Resources School of Earth Sciences and ResourcesChina University of Geosciences(Beijing)Beijing 100083China

Seamount accretion is one of the most significant accretionary orogenic processes in the Central Asian Orogenic Belt,but there are few paleo-seamounts reported from and debate on the tectonic evolution of the Junggar Ocean still *** this study,we present geochronological,mineralogical,geochemical and isotopic data for basalts from the Chagantaolegai ophiolitic mélanges in *** U-Pb dating on one basalt yielded a weighted mean^(206)Pb/^(238)U age of 469±7 Ma,which suggests that it formed in the Middle *** rock samples belong to alkaline basalt and show similar geochemical characteristics,displaying high TiO_(2)(~3 wt%),(La/Yb)N(17.6–19.0),ΣREE(232–289 ppm)and enrichment in Nb and Ta,which implies an ocean island basalt(OIB)*** upon positiveεN d(t)(+4.16 to+4.23),ΔNb(0.20–0.22)and low initial^(87)Sr/^(86)Sr(0.70425 to 0.70452)and Zr/Nb(3.35–3.57),we suggest that the Chagantaolegai OIB samples were likely derived from a fertile mantle source related to *** OIB rock assemblage,chert and marble in the southern part of the Chagantaolegai ophiolitic mélange indicates that a Middle Ordovician seamount was accreted to the Boshchekul-Chingiz arc due to the northward subduction of the Junggar-Balkhash Ocean.

关键词： ocean island basalt seamount Middle Ordovician CAOB West Junggar

Inclusive Growth and Social Fairness

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学术界 2011年第1期 249-250页

作者： chen jiafu school of Marxism ,Shandong University

In the domestic and foreign theoretical study and social practice,social fairness is always *** growth is a result of deep thinking on social *** ultimate purpose of inclusive growth is to spread the benefits of econo... 详细信息

关键词： deep Inclusive Growth and Social Fairness

Geochemistry of Platinum Group and Rare Earth Elements of the Polymetallic Layer in the Lower Cambrian,Weng'an,Guizhou Province

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Acta Geologica Sinica(English Edition) 2009年第3期83卷 618-627页

作者： FU Yong WU Chaodong GUAN Ping QU Wenjun chen jiafu Key Laboratory of Orogenic Belts and Crustal Evolution MOE Peking University Beijing 100871 China National Research Center of Geoanalysis Beijing 100037 China

The black shales of the Lower Cambrian Niutitang Formation in Weng＇an, on the Yangtze platform of south China, contain voluminous polymetallic sulfide deposits. A comprehensive geochemical investigation of trace, rare earth, and platinum group elements （PGE） has been undertaken in order to discuss its ore genesis and correlation with the tectono-depositional setting. The ore-bearing layers enrich molybdenum （Mo）, nickel （Ni）, vanadium （V）, lead （Pb）, strontium （Sr）, barium （Ba）, uranium （U）, arsenic （As）, and rare earth elements （REE） in abundance. High uranium/ thorium （U/Th） ratios （U/Th〉I） indicated that mineralization was mainly influenced by the hydrothermal process. The 8U value was above 1.9, showing a reducing sedimentary condition. The REE patterns showed high enrichment in light rare earth elements （LREE）（heavy rare earth elements （HREE）（LREE/HREE=5-17）, slightly negative europium （Eu） and cerium （Ce） anomalies （δEu=0.81- 0.93）, and positive Ce anomalies （δCe=0.76-1.12）. PGE abundance was characterized by the PGE-type distribution patterns, enriching platinum （Pt）, palladium （Pd）, ruthenium （Ru） and osmium （Os）. The Pt/Pd ratio was 0.8, which is close to the ratios of seawater and ultramafic rocks. All of these geochemical features suggest that the mineralization was triggered by hydrothermal activity in an extensional setting in the context of break-up of the Rodinian supercontinent.

关键词： geochemistry polymetallic layer hydrothermal activity Lower Cambrian

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扁核木不同直径茎干的光合生理特征