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471.
472.
Roberto Stanley Molina–Garza Jim Pindell Diego Villagómez 《International Geology Review》2020,62(4):415-420
ABSTRACTWe discuss the 2018 publication that reports petrographic, heavy mineral data, mineral chemistry, and zircon geochronology for Oligocene sandstones in the Cerro Pelón area in southern Mexico Sureste basin. As the title of their paper says, the goal of their study is to establish the source (s) of the voluminous Cenozoic section in this region, reaching several kilometres in thickness and important as a petroleum system. These authors conclude that Oligocene sandstones of La Laja Formation were mostly sourced from eclogite- to greenschist-facies metasedimentary, metaigneous, and ultramafic rocks of the Guatemala suture complex. Minor contributions from the Chiapas Massif Complex, exposed directly to the south ~60 km of the Cerro Pelón area, were also suggested by the authors. They thus conclude that the Palaeogene stratigraphic record in southeastern Mexico was mostly controlled by the development of the Caribbean–North America plate boundary rather than by orogenic processes at the Pacific margin of North America. Presently, we do not agree with the conclusions of Ortega Flores and colleagues who studied the Cerro Pelón section, thus some discussion is required. Serpentinite bearing Nanchital Conglomerate is well exposed in the Cerro Pelón area, and high- to low-grade metamorphic rocks experienced an uplift in the vicinity of the Cerro Pelón area at the time of deposition of the La Laja Formation. We believe the data are better explained by multiple local sources in southern and eastern Oaxaca as well as sources to the south and southwest, which include the Cenozoic coastal batholith, the Grenvillean/Guichicovi basement complexes, the Chiapas Massif, the Mazatlán schist and other units in the Cuicateco Belt, as well as the Mesozoic cover of these areas (Todos Santos Formation, Cretaceous carbonate rocks, and Paleogene strata such as the Soyaló and Bosque Formations). 相似文献
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云南省单台地震预报6年报准了12次5.2~7.3级地震。总结了反映孕震过程的矢量凹形、应力凹形、地电凹形等3种凹形震兆,阐述了水汞、水氡突跳,形变相关系数和地磁最大相关系数等前兆图像及其预报作用。认为:按照以场求源的思路,追踪孕震过程,是提高地震预报水平的有效途径。 相似文献
475.
牛庄洼陷烃源岩体的几何学描述 总被引:1,自引:0,他引:1
油气资源评价,应该从以构造单元为评价单元,走向以蕴含于构造单元内的生成油气的地质体为单元。界定生成油气的烃源岩体,要综合应用地质、有机地球化学、地球物理等学科从三维空间上来进行。本文以牛庄洼陷为例,具体地使用岩心、测井曲线、古生物化石、有机地球化学指标、地震剖面等资料,描述了沙四上亚段的低熟及成熟烃源岩的几何形态,以及它们在生成演化上的相互联接。 相似文献
476.
鄂尔多斯盆地中部气田奥陶系风化壳气藏天然气来源及混源比计算 总被引:19,自引:4,他引:15
对鄂尔多斯盆地中部气田天然气碳同位素资料按不同地区、不同层位进行了分析,认为奥陶系风化壳气藏甲烷碳同位素值与石炭-二叠系气藏的接近,在平面上变化趋势相似,而与风化壳之下奥陶系自生自储的油型气相差较大。奥陶系风化壳气藏的来源是以石炭-二叠系煤成气为主,定量计算表明,在中部气田的大部分地区,石炭-二叠系来源气的比例大于70%。 相似文献
477.
华北克拉通不同时代基性火山岩存在向富集方向演化的趋势,并出现明显的Ar-Pt界限和新生代异常.元古宙基性火山岩比太古宙富集大部分高场强元素(HFSE)和轻稀土元素(LREE),REE分异程度显著增加,而且相容性接近的不相容元素(如Nb,Ta)的相对不相容性发生了改变.新生代玄武岩HFSE及Ni高度富集,REE强烈分异,δ(Eu)值最高.Ar-Pt界限可能与地幔熔融时物理条件(如氧逸度)的改变和地幔富集作用有关.新生代玄武岩独特的地球化学特征可能主要反映了地幔源区的特殊性———“似OIB型”富集地幔,其形成既可能有携带远洋沉积物的俯冲古老玄武岩洋壳部分熔融残余的贡献,也可能有直接循环(如通过拆沉作用)的陆壳物质的贡献,同时还可能涉及了地幔柱活动的影响. 相似文献
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479.
云南金厂金矿床蚀变超基性岩体与金的成矿作用 总被引:10,自引:0,他引:10
金矿化与蚀变超基性岩体的空间关系、矿化特征、蚀变超基性岩体、成矿流体、微量元素、硫同位素组成、表明金主要来源于金厂蛇纹石化、滑石化、碳酸盐化超基性岩体。在岩体蚀变过程中,在碱性相对还原的介质条件下,金主要以硫络合物的形式进入成矿溶液,在T、P、PH、Eh等物理化学参数发生变化的条件下沉淀。 相似文献
480.
气候系统内极区热汇与热带海洋热源之间的相互作用(英) 总被引:2,自引:1,他引:1
The anomalous change of two polar sea ice and tropical ocean SST is a very important index for global climate monitoring and prediction. In this paper, the wave resonance principle is used to calculate month by month running cross couple correlation coefficient time series between sea ice in different sea area of two Polars, as well as between them and five elements of E1 Nino events, to analyze their variation features, and to find out their resonance periods. The resonance period of two waves is just the strongest interaction period.Some results are concluded as follows. 1) The Arctic sea ice to the Pacific-side (NPI1) and Atlantic-side (NP12) show a strong positive-negative feedback impact each other to the Antarctic Ross Sea ice (SPI2) with equal intensity. 2) Both NPI1 and NPI2 give a strong positive and negative feedback to the Antarctic Wedded Sea ice (SPI3) while it is rather weak in convercse status. It means that, the Arctic sea ice plays a leading and controlling role on the Wedded Sea ice. 3) SST of Nino 4 area in thecentral equatorial Pacific has a best resonance period with SPI2 with cycle period of 132 months. It closely relates to quasi-11 years oscillation period of both SST of Nino 4 area and SPI2. SST of Nino 4 has also a resonance period to SPI3 with cycle of 61 months. There also exist strong interaction periods between the Antarctic sea ice and other elements of ENSO event but weaker than SST of Nino 4 area. 相似文献