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| 1 | Research advances in the Mesozoic tectonic regimes during the formation of Jiaodong ore cluster area显示文摘在诺思中国的东方区域在中生代时代在 Jiaodong 矿石簇区域和相关构造政体转变把构造政体的进展基于研究,在这篇论文,我们首先总结要求后面被学习的一些关键问题。然后,我们建议一条途径到处理这些问题。在 Jiaodong 矿石的金存款聚类区域,这被知道,它具有不同矿化作用式样,空间 istributions 和地质的背景,可能作为从在中生代的至少一个地质的事件的结果。到现在为止,特别在上述事件的 geodynamic 机制上,关于时间的进化和空间迁居顺序的这种研究是远非足够的。而且,描述行动模式和构造动态政体的时间空间的框架并且提出每构造动态政体的相对贡献因为 metallogensis 是静止的质问到地质学家在 Jiaodong 的形成上学习的份量上矿石簇区域。根据地区性的构造分析,结构的动力学,观察和矿化作用网络的探索的解释,我们建议有一些的一个 geological-physical-chemical 模型抑制从全面分析发源。我们然后使用这个模型模仿结构的变丑,热运输,液体流动和化学反应的联合过程。获得的结果显示模型在进一步在 Jiaodong 矿石簇区域并且在进一步理解集体 metallogensis 的性质分析构造政体的时间空间的进化小道是有效的。 | DENG Jun YANG Liqiang GE Liangsheng WANG Qingfei ZHANG Jing GAO Bangfei ZHOU Yinghua JIANG Shaoqing | 2006 | Progress in Natural Science:Materials International2006，16，8： | 51 |
| 2 | Metallogenic epoch and genesis of the gold deposits in Jiaodong Peninsula, Eastern China: a regional review显示文摘金存款被多来源,重迭,大规模和时间空间的集中在 Jiaodong 半岛描绘,东方中国。在这篇论文,我们在 metallogenic 年表和金存款的开始上考察历史和学习的发展,总结附加 metallogenesis 的主要特征,提供中生代复杂 metallogenic 系统的证据,并且从一个地区性的看法为 Jiaodong 金存款簇的进一步的研究指出一些问题。尽管金存款在基因类型,形成矿石的材料和地质的背景是不同的,我们的研究显示形成矿石的材料的累积和炮兵阵地 temporally 空间地被专注于大规模,和 Jiaodong 金存款的主要 metallogenic 时代在中生代被集中。Metallogenic 年表和 geological-geochemical 数据显示有金矿化作用的二个时期在 Jiaodong 分别地发生在 130-110 妈和 90-80 妈矿石簇。从 polygenetic 矿化作用的重迭的金存款簇结果,和进一步的学习被需要调查中生代复杂 metallogenic 系统的形成和进化。 | YANG Liqiang DENG Jun GE Liangsheng WANG Oingfei ZHANG Jing GAO Bangfei J IANGShaoqing XU Hao | 2007 | Progress in Natural Science:Materials International2007，17，2： | 30 |
| 3 | Reconstruction of Ore-controlling Structures Resulting from Magmatic Intrusion into the Tongling Ore Cluster Area during the Yanshanian Epoch显示文摘摘要:Tongling 矿石簇区域经历了集中的压缩并且联系了在 Indosinian-Yanshanian 时代期间砍,它形成了一个箱子在 caprock 的控制矿石的褶层和差错系统。在 Yanshanian 时代的 magmatic 侵入导致了多相的液体的多级式的 unmixing,导致多层、宽范围、多种形式的式样描绘的矿化作用。在 Tongling 区域的 magmatic 侵入不仅供应了必要形成矿石的材料,而且重建控制矿石的结构根据下列五条阶层边界的趋势表面模拟:志留纪泥盆纪,泥盆纪含碳,含碳二叠,中间二叠上面二叠、二叠三叠纪。这模拟的结果证明那在那里存在在上面的部分和那些在的阶层之间的重要差别更低。而上面的趋势表面是 synform,更低的趋势表面是 antiform。另外,趋势迭加邻近的床边界出现(例如,志留纪泥盆纪边界在泥盆纪含碳的边界之上迭加) 证明更低的趋势表面总是上面穿透那。而且,不同迭加的趋势表面的穿透的部分的位置和取向是类似的并且根据地区性的 E-W-trending magmatic-metallogenic 带的分发显示出 E-W-trending 带的分发。基于阶层,结构的变丑机制,和地现象的机械性质的全面分析,看起来, stratal 趋势表面的特殊特征由于 magmatic 侵入源于 jacking 进一个 E-W-trending 地下室差错以前控制的 caprock。因此,主要控制矿石的结构,在地区性的水平压缩期间形成了,被形成矿石的岩浆的垂直 jacking 功能在 Yanshanian 时代期间重建,这被推出。在形成矿石的过程期间,岩浆的本地垂直 jacking,结合了地区性的水平压缩,在液体水管网络优化了广泛的环境并且加速了多相的液体的 unmixing 后面的 magmatic 炮兵阵地。Jacking 也加强了垂直、侧面的指导液体的结构,供应为多层的炮兵阵地和多相的液体的广阔运输的更合适的物理条件。 | DENG Jun WANG Qingfei YANG Liqiang GAO Bangfei HUANG Dinghua LIU Yah XU Hao JIANG Shaoqing | 2007 | Acta Geologica Sinica(English Edition)2007，81，2： | 13 |
| 4 | Tectonic Constraints on the Transformation of Paleozoic Framework of Uplift and Depression in the Ordos Area显示文摘During the Paleozoic, the Ordos area in the western North China Plate was located at the intersecting position of microplates and controlled by their interaction. The structural framework in the Ordos area, which underwent transformations in the Ordovician, the Carboniferous and the Permian respectively, was dominated by the alternation of uplift and depression. The transformations of structural framework are utilized as the clues to investigate the microplates’ interacting type and its response in the Ordos area. According to the regional structural evolution, the Ordos area is simplified into an isopachous, isotropic and elastic shell model, and under proposed various boundary conditions, three series of numerical simulations corresponding to the three structural transformations are carried out to determine the detailed tectonic constraints. Numerical simulations reveal that the structure of the uplift and depression, which is similar to the actual pattern, develops only under one special boundary condition in each of the three series, indicating that the structural framework responds to the unique tectonic background. The simulation results show that in the Early Paleozoic, the L-shaped paleouplift formed nearby the southwestern corner of the Ordos area because the intensity of the compressions in the southern and western boundaries resulting from the ocean-continent collisions was similar. In the Late Paleozoic, it evolved into continent-continent (or arc-continent) interaction in the southern and northern boundaries; in the preliminary stage of the interaction, since the interface between the North China Plate and the plates on the south and north was narrow, the relative acting force was little and the regional western boundary immobile, and the structural framework in the basin was characterized by the N-S trending slender-waist-shaped uplift; as the interface between the plates expanded gradually, the extrusive force in the southern and northern boundaries of the North China Plate increased, resulting in the paleogeographic divisions showing E-W trending, and, the western boundary of the basin was extruded westward due to the intense compression inducing the local NE trending of paleogeographic division in the central area. The simulation results further reflect that the symmetry of the uplift-depression pattern is restricted by that of the boundary conditions, suggesting that the Paleozoic structural transformations of the Ordos area under boundary constraints accord with the universal physical symmetrical principle. | WANG Qingfei DENG Jun HUANG Dinghua YANG Liqiang GAO Bangfei XU Hao JIANG Shaoqing | 2006 | Acta Geologica Sinica(English Edition)2006，80，6： | 10 |
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