“中国之治”的制度优势

党的十九届四中全会站在党和国家事业全局和战略高度,立足当前,着眼长远,专门研究审议了坚持和完善中国特色社会主义制度、推进国家治理体系和治理能力现代化的重大问题,从坚定制度自信和推进制度创新的结合上系统回答了“坚持和巩固什么、完善和发展什么”这个重大政治问题,第一次集中概括了中国特色社会主义制度有机联系、相辅相成、汇聚整体的显著优势,系统阐述了由根本制度、基本制度、重要制度构成的层次清晰、全面系统的科学制度体系,明确提出了推进我国制度建设和国家治理的指导思想、总体要求、总体目标、战略途径和重大举措。这次全会通过的《中共中央关于坚持和完善中国特色社会主义制度推进国家治理体系和治理能力现代化若干重大问题的决定》(以下简称《决定》)A,充分体现了以习近平同志为核心的党中央对中国特色社会主义建设规律认识的深化,对科学社会主义理论与实践的丰富发展,为成功实现“中国之治”提供了深厚的制度基础和有力的制度保障。     

阆中大像山石窟的形制、题材与时代

位于四川省阆中市的大像山石窟,主要开凿于中晚唐和宋代,明清时期也有少量开凿。现有37龛,以方形龛、外方内圆拱形龛及圆拱形龛为主,方形龛最为多见。龛楣大多无装饰,雕刻简单。题材主要有弥勒佛、七佛、千佛、观音、天王、力士、经幢及舍利塔等。造像组合较少,以单身造像为多。阆中独特的地理位置,使得大像山石窟兼具广元、巴中两地石窟的特点,其丰富的内容为巴蜀佛教石窟寺的深入研究提供了重要的实物资料。     

Earthquake Resilience of Reinforced Concrete Structural Walls with Replaceable “Fuses”

The concept of providing a fuse in a structural system has been both developed and investigated over the past few years (e.g., the use of replaceable links in eccentrically braced frames or the use of replaceable links in the new San Francisco-Oakland Bay Bridge). This paper presents a new coupling beam with a creative fuse installed in the mid-span of a steel-concrete composite beam via an end plate and high-strength bolts. First, a practical design methodology of a replaceable coupling beam is presented. Next, the seismic behavior of the proposed fuse is tested and evaluated, and two structural wall specimens with or without a fuse are designed and fabricated according to the proposed design methods. The two specimens possess similar shear capacities under large-scale cyclic loading, and the walls of the two specimens show similar failure modes; however, the new walls exhibit slightly lower levels of damage than the conventional walls. In particular, the inelastic deformation and damage of replaceable coupling beams are mainly concentrated in the fuse, whereas the non-yield segment and the beam-wall pier interfaces remain nearly intact and produce only slight damage, which is beneficial regarding the replacement of the fuse in post-earthquake events.     

Fluid mixing induced by hydrothermal activity in the ordovician carbonates in Tarim Basin,China

Permian hydrothermal activity in the Tarim Basin may have been responsible for the invasion of hot brines into Ordovician carbonate reservoirs. Studies have been undertaken to explain the origin and geochemical characteristics of the diagenetic fluid present during this hydrothermal event although there is no consensus on it. We present a genetic model resulting from the study of δ¹³C, δ¹⁸O, δ³⁴S, and ⁸⁷Sr/⁸⁶Sr isotope values and fluid inclusions (FIs) from fracture‐ and vug‐filling calcite, saddle dolomite, fluorite, barite, quartz, and anhydrite from Ordovician outcrops in northwest (NW) Tarim Basin and subsurface cores in Central Tarim Basin. The presence of hydrothermal fluid was confirmed by minerals with fluid inclusion homogenization temperatures being >10°C higher than the paleo‐formation burial temperatures both in the NW Tarim and in the Central Tarim areas. The mixing of hot (>200°C), high‐salinity (>24 wt% NaCl), ⁸⁷Sr‐rich (up to 0.7104) hydrothermal fluid with cool (60–100°C), low‐salinity (0 to 3.5 wt% NaCl), also ⁸⁷Sr‐rich (up to 0.7010) meteoric water in the Ordovician unit was supported by the salinity of fluid inclusions, and δ¹³C, δ¹⁸O, and ⁸⁷Sr/⁸⁶Sr isotopic values of the diagenetic minerals. Up‐migrated hydrothermal fluids from the deeper Cambrian strata may have contributed to the hot brine with high sulfate concentrations which promoted thermochemical sulfate reduction (TSR) in the Ordovician, resulting in the formation of ¹²C‐rich (δ¹³C as low as ?13.8‰) calcite and ³⁴S‐rich (δ³⁴S values from 21.4‰ to 29.7‰) H₂S, pyrite, and elemental sulfur. Hydrothermal fluid mixing with fresh water in Ordovician strata in Tarim Basin was facilitated by deep‐seated faults and up‐reaching faults due to the pervasive Permian magmatic activity. Collectively, fluid mixing, hydrothermal dolomitization, TSR, and faulting may have locally dissolved the host carbonates and increased the reservoir porosity and permeability, which has significant implications for hydrocarbon exploration.     

地方发展变迁与居民地方感关系研究——以广州荔枝湾涌历史文化街区为例

本文以广州荔枝湾涌历史文化街区为例,运用扎根理论研究荔枝湾涌1940年代以来地方发展变迁与居民地方感的关系,进而挖掘居民地方感变化机制。研究发现：荔枝湾涌居民的地方感主要受生态环境、建筑与配套服务、集体记忆、活动类型、人际关系等因素的影响,其中生态环境起主导性作用;积极地方感主要来源于集体记忆的保留与延续;消极地方感主要来源于破旧的居住环境及落后的配套服务;此外,文章提出内向型地方感和外向型地方感的概念,认为随着城市发展,在地方发展变迁过程中,地方感由内向型地方感转变为内向型和外向型相结合的地方感。两种地方感相互作用,互相调节,更有利于地方稳定、开放、包容地发展。     

试析夏商西周文化和冀西北、京津唐地区北方青铜文化的关系

夏商西周文化对冀西北、京津唐地区北方青铜文化格局的变迁具有重要影响.夏文化与这个地区的北方青铜文化存在间接的联系;商文化向北的扩张与收缩极大地冲击了这个地区原有的文化格局;西周文化对这个地区的文化渗透最终使得这个地区纳入了中原青铜文化区.     

辽金元三代懿州治所考

本文根据文献与考古资料,认为辽越国公主槊古公主以从嫁户所建的头下城懿州即今辽宁阜新塔营子古城.改为行政州以后,懿州下辖宁昌、顺安两县,顺安就是塔营子古城,宁昌即塔营子北10公里的平安地古城.辽代末年,将懿州州治从顺安迁到了宁昌.金皇统三年(1143年)又将宁昌省入顺安,州治也迁回了顺安,此后至元代,没有变化,懿州州治一直在塔营子古城.     

汉简中所见的河西开发及启示

河西地区地域辽阔,土地广袤,我们的祖先从远古时期就开始开发这片土地,两汉时期,开发活动达到了一次高潮.汉代对西北的开发主要采取徙民实边和戍守屯田两种措施.我们力图从史书和汉简中找到一些原始材料,管窥当年开发西北的真实状况,为今天开发西北的活动提供一些经验及借鉴.     

孟善不是华容人——明万历《华容县志》勘误一则

本文通过《明史》、《皇明人物考要》以及档案资料相关明代保定侯孟善的记载,考证孟善不是华容籍人士,从而更正了明万历《华容县志》中的错误。     

日本人历史认识问题的症结点

如何看待日本近代历史,尤其是对外战争历史,在日本社会一直是一个有极大争议的问题。本文即从日本的基本政治立场、影响国民的无构造史观、战后的反省程度以及片面的被害意识等方面,分析日本人历史认识问题的症结所在。