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Gray crystalline hematite on Mars has been detected in three regions, Sinus Meridiani, Aram Chaos, and Valles Marineris, first by the Thermal Emission Spectrometer (TES) onboard the Mars Global Surveyor (MGS) orbiter, and then confirmed by other instruments. The hematite-rich spherules were also detected by the Mars Exploration Rover (MER) Opportunity at Meridiani Planum (Sinus Meridiani). Formation mechanisms of the hematite-rich spherules have been discussed widely since then. Here, we argue for an alternative formation mechanism, that is, the spherules originally formed at Valles Marineris due to the interaction of volcanic deposits and acidic hydrothermal fluids, and then were transported to and deposited at Meridiani Planum and Aram Chaos as alluvial/fluvial sedimentary deposits with other materials such as sulfates and rock fragments during the wash-out flows from Valles Marineris to Meridiani Planum and Aram Chaos. Diagenesis of the hematite-rich spherules may have also been a possible mechanism following sediment transport and emplacement. The hypothesis is consistent with available relevant information to date and provides an insight into the understanding of Martian surficial processes. 相似文献
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一个多世纪以来经历过几代人的不懈努力,尤其是近年来岩浆不混溶作用在业界得到重视,使其理论研究和实践运用都达到了前所未有的高度。笔者在中国东南沿海火山岩中首次发现大规模酸性岩浆不混溶现象,通过详细的岩相学研究揭示,大约温度在900~650℃之间、剧烈的过冷度变化条件下岩浆发生不混溶两液相,一相为富硅的球粒相,另一相为富铁的基体相。不混溶球粒相发展,最初可能由大黏度富桥氧的硅氧四面体-络阴离子团聚集成核,成核后形成珠滴状液滴,液滴聚集成塑性小球,小球碰撞合并奠定球粒个体,球粒个体先后经历过三个世代的反复交叠生长而定型。在浮力和岩浆上侵的综合作用下,无数个球粒个体与熔浆分离、上浮、云集成规模宏大的富硅球粒相,即球粒流纹斑岩地质体,富铁基体相下沉形成英安岩地质体。地球化学特征表明,球粒相富集主元素SiO2、K2O、Na2O和微量元素Sr、Ba;基体相富集主元素Al2O3、TiO2、MgO、TFe2O3和微量元素Rb、Cs... 相似文献
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SONG Tianrui HE Zhengjun WAN Yusheng LIU Yanxue 《《地质学报》英文版》2007,81(4):649-657
Numerous iron cosmic micro-spherules have been discovered from Mesoproterozoic strata including the Changzhougou Formation(1.8 Ga) and the Dahongyu Formation(1.6 Ga) of the Ming Tombs district,Beijing.There are 1 to 30 grains of cosmic spherules per 2 kg of a sandstone sample taken from the bottom of a coarse sandstone bed of the Changzhougou Formation and 56 grains per 3.69 kg of a rock sample from silicified carbonate rocks of the Dahongyu Formation.The surface textures of cosmic spherules analyzed by means of the secondary electron imagery are identical with those reported from references either domestic or abroad.So far the geo-ages of 1.8 Ga and 1.6 Ga of cosmic spherules from the Changzhougou and Dahongyu formations might be older than those reported in the world.Table 1 gives the electron probe analysis data of cosmic spherules for 30 spherule grains and 44 testing points as follows(%):FeO,80-95;Cr_2O_3;0-9.56;NiO,0-0.78;CoO,0-0.46; indicating that the Cr_2O_3 content is higher and FeO content lower in the Changzhougou Formation than in the Dahongyu Formation.The helium isotopic data of cosmic spherules as well as their host rocks vary greatly between the Changzhougou and the Dahongyu formations as shown in Table 2.The data of cosmic spherules of the Changzhougou Formation vs the Dahongyu Formation are 57.5/1.23 in ~3He/~4He(10~(-8));and 55.54/809.60 in ~4He(10~(-6)cm~3STP/g);those of coarse sandstone of the Changzhougou Formation vs silicified carbonate of the Dahongyu Formation are 3.39/2.59 in ~3He/~4He(10~(-8)) and 4.56/2.34 in ~3He(10~(-6)cm~3STP/g).The ratio of analytic data of helium isotopes are different for cosmic spherules and their host rocks;for example,the ~3He/~4He(10~(-8)) values are 16.96 and 0.48,and the ~4He (10~(-6)cm~3STP/g) are 12.18 and 345.98 for the Changzhougou and Dahongyu formations respectively.It was reported that the world's oldest micrometeorites had been found in the Meso-Proterozoic Satakunta Formation,Finland.However,the cosmic spherules from the Meso-Proterozoic Changzhougou and Dahongyu formations are 200 to 400 Ma older than those from the Satakunta Formation.Besides,one carbonaceous chondrite grain was discovered for the first time as the earliest remain formed in the solar nebula from the Dahongyu Formation. 相似文献
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