塔里木东部满东1井志留系天然气成因与成藏期初步分析

满东1气藏的发现是塔里木盆地东部地区油气勘探获得新突破的重要标志。本文充分利用目前所获得的大量地质和地球化学资料,从天然气的组份特征、成因类型、成熟度和气源对比等方面对该井天然气的成因进行了分析,认为满东1井天然气属于海相腐泥型天然气,来源于寒武系-下奥陶统海相过成熟烃源岩,烃类气体组成具有油裂解气的特征。海相泥质烃源岩中氨基粘土矿物在过成熟阶段分解并氧化,形成大量的氮气,导致满东1气藏高含氮气。包裹体和埋藏史研究结果表明满东1气藏成藏过程复杂,主要成藏期为燕山喜马拉雅期。     

花岗岩块状样品的熔融实验研究

以粉末样品的熔融实验为基础的花岗岩体系相平衡理论，在花岗岩成因研究方面具有一的局限性。天然花岗岩块关样品的熔融实验表明，赋存于矿物颗粒间的熔体成主主要受控于不同矿物边界的局部熔融体系。较低温条件下的熔体基本属于花岗岩体系的低熔点成分，而较高温度下的熔体则远离同熔线转变为非平衡熔体。     

Craton destruction and related resources

International Journal of Earth Sciences - Craton destruction is a dynamic event that plays an important role in Earth’s evolution. Based on comprehensive observations of many studies on the...     

Tectonic setting of the Helong Block: Implications for the northern boundary of the eastern North China Craton

The Helong block, located in southeastern Jilin Province, was thought to be an Archean geological unit in the most northeast part of the North China Craton (NCC)[1,2]. Previous geological survey sug-gested that this block is mainly composed of two parts: Jinchengdong Archean metamorphic supracrustal rocks intruded by Archean TTG complex[3―5], and the Bailiping granite[6,7] distributed in the Shiliping-Bai- liping-Guangping area. Both of them were thought as the Jinchengdong (or Helong…     

清代县级行政区划调整的时空变动与演化机理

行政区划是国家治理体系的重要组成部分,系统分析清代县级行政区划调整的时空变动格局和影响因素,能更好地借鉴和发挥行政区划设置在国家与地方治理中的支撑作用。综合梳理国家清史纂修工程《清史·地理志》的考证结果,参考中国第一历史档案馆藏清代档案、《清实录》《清会典》《大清一统志》以及清代地方志等历史文献,全面分析1683—1911年中国县级行政区划的时空变动过程与演变规律。研究表明：① 清代县级行政区划主要有9类调整模式,以自下而上的申报调整为主,关键是总督和巡抚的提议权,督抚体制是行政区划调整推进的制度保障;② 行政区划调整的频次受最高统治者的治理理念影响较大,波动明显,雍正朝是清代行政区划调整的绝对高峰期,光绪和宣统两朝是一个相对高峰期,道光、咸丰到同治时期调整最少;③ 县级行政区划的调整以新设最多,其次为改隶和析分,同级变更和合并是频次较少的两类调整;④ 升级、迁治、裁撤、新设4类调整在清代23个省的分布范围较广泛、各省域分布较为广泛均衡,变更专名、合并、改隶、同级变更4类调整的分布范围集中于直隶、河南、山西等省;⑤ 清代县级行政区划调整格局的形成与演化是多方面因素共同作用的结果,政治安全和统治方便是决定性因素,总体上体现出层级明确、权责明晰、因地制宜、循序渐进的国家治理理念。     

一种震前超低频密度——应力波

地震发生前天文时纬残差观测数据出现异常,得到了不同天文台观测结果的证实。另外,两种与地震相关的物理量震前地下深部物质视电阻率变化和断层活动矩变化,其物理机制的解释以及与后续地震的关联方式和天文时纬残差有很多共性。而且,这3类观测现象与后续地震的关联方式与国外学者提出的热力学弹性回跳模型符合得很好。本文基于现有观测证据和理论模型的一致性,提出地震前在地层构造中存在一种来自孕震区域的超低频密度—应力波。     

Fractal characteristics of resource quantity of cobalt crusts and seamount topography, the West Pacific

This paper presents the fractal distribution of topography of seamounts from the West Pacific and the resource quantity of cobalt crust therein. The cobalt resource quantity has three to four variable fractal dimensions, corresponding to the distinct slopes and water depths of the seamount. The multiple fractal property of resource quantity may have resulted from various factors, such as types and components of cobalt crusts and ages of oceanic crusts hosting the seamounts. Individual seamounts display complex topography and quantity of cobalt crust, both in the same and different regions. Translated from Acta Sedimentologica Sinica, 2006, 24(5): 705–713 [译自: 沉积学报]     

Aeolian Deposits in the Yarlung Zangbo River Basin,Southern Tibetan Plateau: A Brief Review

The Yarlung Zangbo River is located in the southern Tibetan Plateau. Loess since the geological history and modern aeolian sand dunes are widely developed in the basin, bearing rich information on the aeolian processes and environmental evolution. In this work, we reviewed the main research progress of aeolian deposits in the Yarlung Zangbo River basin in recent years, and discussed the distribution characteristics, accumulation age, sediment characteristics and provenance and the possible formation mechanism of aeolian deposits and the history of aeolian activity. The results show that loess is mainly developed on the river’s terraces and some of the hilltops, and mostly formed since the last glacial maximum and mainly developed since Marine Isotope Stage 1 (about 14 ka BP), while aeolian sand deposit is mainly developed in the river’s wide valley, with relatively short accumulation time. The sediment particles mainly underwent mechanical transport and physical weathering, but chemical weathering was weak. Although the physical and chemical properties of sediments show some spatial changes, there still exist obvious local characteristics, which are closely related to the nearby surface sediments. Under the background of aeolian source, the local-source genesis of loess is generally recognized. The surface loose material at the bottom of valley is main material source of aeolian deposits. The evolution of aeolian activity is relatively complex. In addition to the regional climate change, the local environment is also an important factor affecting the aeolian activity and its regional difference. Based on the previous studies, we suggest that the systematic study on the physical and chemical properties of aeolian sediments, climate change since the Holocene and the impact of dust emission on human living environment should be strengthened in the future research.     

吉林南部太古宙辉石花岗岩的成因

吉林南部太古宙辉石花岗岩类具有与英云闪长质－奥长花岗岩质－花岗闪长质片麻岩（ＴＴＧ）及深熔钾长花岗岩不同的特征，并不是ＴＴＧ岩系的一部分。地质学、岩石学及地球化学研究表明，该辉石花岗岩类是壳源岩浆结晶分异作用的结果，其岩浆演化主要受早期结晶的辉石、斜长石及角闪石等矿物相的制约。     

On the Upper Pleistocene Lamellibranchiate fossil groups and paleo-oceanic environment of the Huanghai Sea

Research on Lamelllbranchiate fossils of the Huanghai Sea started rather late in China and data on this subject are scarce. During the large-scale investigation of the Huanghai Sea sediment in the late 1970s, a large number of surface and core samples of the sea-floor sediment were obtained and a considerable number of Lamellibranchiatc fossils were found. A preliminary identification reveals that there are 46 species of the fossils.The Lamellibranchiate fossils in the Huanghai Sea are composed of different species: the shallow water species, the littoral species and the fossils reflecting the environment of the estuary where freshwater flows, or of the tidal zone having brackish water.Through the studies of the Lamellibranchiate fossils and their ecological environment, not only the features of the Lamellibranchiate groups of the Upper Pleistocene have been restored, but also some relatively important data of the investigation of paleo-current and paleo-temperature during late Pleistocene have been obt