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71.
72.
R.M. Hernndez T.E. Jordan A. Dalenz Farjat L. Echavarría B.D. Idleman J.H. Reynolds 《Journal of South American Earth Sciences》2005,19(4):495-512
Marine transgression onto the South American continent took place at least twice in the Miocene along distinct paleogeographic corridors. The first event occurred between 15 and 13 Ma and the second between 10 and 5? Ma. Each event has particular dominant variables (tectonism, eustacy, sediment accumulation rate) that permitted the preservation of the record and development of the sea on the continent. The 15–13 Ma transgression was tectonically and eustatically controlled, flooding older sedimentary accommodation zones on the South American plate during a global high sea level, whereas the 105? Ma event was predominantly tectonically controlled, generated by tectonic loading created in the Cordillera Oriental fold-and-thrust belt. A new 7.72±0.31 Ma 40Ar/39Ar date from the Río Parapetí in Bolivia suggests that the 15–13 Ma transgression registered in Argentina produced no continental connection to the Caribbean transgression, registered in Bolivia, because of temporal constraints. 相似文献
73.
In the Bengal Delta Plain (BDP) the primary arsenic sourcing appears to be different from the global scenario. Here, the Terminal Pleistocene–Holocene depositional platform, the interactive early Holocene depositional morphology with fluvio-estuarine and marine incursions played a crucial role for arsenic sourcing and enrichment. The lenticular silt-fine sand layer between anoxic clay beds favoured entrapment of dissolved organic carbon with decayed phyto-planktons debris. The Terminal Pleistocene–Holocene transgression and regression processes may have acted as major events in the BDP. Interestingly, at the end of the last glacial maxima, the Pleistocene delta had undergone block movements, wherein some parts of the platform were raised above the level of Holocene deposition. Those blocks were found to be free from arsenic in the groundwater. The sea, during re-emerging inundation (10–7 ka BP), has witnessed a monsoon-induced environment in the BDP with the resultant oscillation of sea level leading to higher upsurge towards the north. This might have resulted in the marine incursion and inundation in pre-existing land depressions. Meanwhile arsenic entrapments through marine incursion as well as enrichment in the presence of organic carbon/DOC and/or Fe/Mn/Al catalytic agents could have developed into localised redox traps. It may be of relevance that due to the repetitive transgressive–regressive phases in Holocene, resulting in periodic exposure and weathering of iron-bearing minerals and consequent iron enrichment in the aquifer system. The iron, thus present, had free charge to host arsenic as a sink. It appears that arsenic, wherever found, would likely be of atypical localised exhaustible phenomenon, both in horizontal and vertical context. It also rationalises the cause of the absence of arsenic in the other nearby Pleistocene platform, which has not come across Holocene interaction and marine incursion, as to the likely limiting condition for the search for arsenic in the BDP or beyond. 相似文献
74.
Jing Li Chang-ling Liu Neng-you Wu Xiao-qing Xu Gao-wei Hu Yan-long Li Qing-guo Meng 《China Geology》2022,5(2):285-292
Large amounts of gas hydrate are distributed in the northern slope of the South China Sea, which is a potential threat of methane leakage. Aerobic methane oxidation by methanotrophs, significant methane biotransformation that occurs in sediment surface and water column, can effectively reduce atmospheric emission of hydrate-decomposed methane. To identify active aerobic methanotrophs and their methane oxidation potential in sediments from the Shenhu Area in the South China Sea, multi-day enrichm... 相似文献
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我国古生代海相碳酸盐岩成藏理论的新进展 总被引:1,自引:0,他引:1
近年来在中国古生界新发现大中型油气田40多个,其中大型油气田16个。在长期研究中国古生代海相沉积特征的基础上,总结归纳近几年来新发现的海相烃源岩,提出对碳酸盐岩有效烃源岩的新认识。从有效烃源岩、古岩溶储集体、油气成藏期次和成藏模式等四个方面概述油气成藏理论方面的新进展;根据油气成藏史研究,结合区域构造演化史、生烃史等,提出塔河油田奥陶系有四个成藏期:加里东中晚期至海西早期;海西晚期;燕山期-喜马拉雅早中期;喜马拉雅晚期。 相似文献
77.
我国部分地区地质灾害爆发频率高,多年来崩滑坡、泥石流等高危险性地质灾害严重威胁我国人民财产与生命安全。因此,地质灾害及时预警一直是我国在应急方面亟待解决的难题。随着北斗、GPS等全球卫星导航系统的建设组网,GNSS技术逐渐成为当前提供时空位置信息的重要手段,具有数据实时性、设备低功耗、搭建便捷化等特性,成为解决地质灾害监测与预警的理想技术手段。本文利用BDS+GPS+GLONASS时空信息数据,构建了面向地质灾害监测的中长基线毫米级精度的崩滑坡监测解算方法,确定了双差观测的载波相位解算模型。最后在重庆新浦区域展开试验应用,实现了基于高精度时空信息的毫米级滑坡灾害的监测与预警。为预计该区域的地质灾害提供了数据支持,为人民的生产生活提供了技术保障。 相似文献
78.
羌塘盆地油气勘探前景展望 总被引:4,自引:0,他引:4
羌塘盆地为中生代大型的海相残留型构造盆地。盆地的南北缝合带及中央隆起带,宏观上可视为三条构造活动带,其间所夹持的两个相对稳定的地块,特别是南、北坳陷中部的两个复向斜区,是油气勘探的主攻方向。上三叠统—上侏罗统是盆地内的沉积主体,“两坳夹一隆”的古构造格局控制了沉积和烃源层的发育和展布。生物礁、滩多分布在高隆起周缘的碳酸盐岩台地上,发育于各组段中,但以侏罗系布曲组及索瓦组相对集中。盆地内发育有上三叠统肖茶卡组、中侏罗统布曲组和夏里组以及上侏罗统索瓦组四套主要烃源层,估算盆地的总生烃量为9930.92×108t,远景资源量为52.95×108t,具有雄厚的找油物质基础。盆地内发育了四套生储盖组合,其中以侏罗系(组合Ⅲ)布曲组—夏里组亚组合最好,是盆地主要的勘探目的层。应用多种方法综合研究和评价认为,北羌塘坳陷金星湖—东湖—托纳木地区和南羌塘坳陷比洛错东—土门地区是最有利的含油气远景区。 相似文献
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80.
汶川大地震对地质环境影响很大,由于大地震的影响,其震前震后的地质灾害类型、数量等发生了很大的改变。本文通过搜集前人资料,现场调查,分析了汶川大地震前后汶川县地质灾害的变化。结果表明,地震前汶川县地质灾害类型主要以泥石流为主,地震后,汶川县地质灾害类型主要为崩塌,其次为泥石流和滑坡。地震使汶川县地质灾害数量极大增加,同时,也使得其主要地质灾害类型发生改变。 相似文献