含大量石英颗粒的就不是陨石吗？

qgs

东方明珠 发表于 2014-12-29 09:16
版主好！你说的地球以外的星球没有石英，这是你的你的定论还是哪个科研机构的定论？告诉大家

楼主您好！这是人类从开始发现陨石种类至今所形成的有根有据的科学的结论！中外众多陨石专家和天文学家以他们坚持不懈的科研工作中所得到的事实！仅此而已！祝您快乐！安康！好陨连连！

星缘之家

东方明珠 发表于 2014-12-26 09:31
内蒙你好！谢谢指点，希望你继续参与讨论。既然石英是在水环境下形成的，那么就证明这种陨 ...

也可能是掉落水里，年代久远，在地球上形成也说不定

兰石园主

自从“机遇”号登上火星后，发现火星曾经有水存在，一些人还死抱着“有石英的就不是陨石”这个陈腐的观点不放吗？

匡长

陈宏毅,缪秉魁,谢兰芳,夏志鹏. 2015. 南极月球陨石MIL05035矿物学、岩石学及演化历史. 岩石学报, 31(4): 1171-1182
南极月球陨石MIL05035矿物学、岩石学及演化历史
作者        单位        E-mail
陈宏毅         桂林理工大学, 广西隐伏金属矿产勘查重点实验室, 桂林 541004
桂林理工大学地球科学学院, 桂林 541004         
缪秉魁         桂林理工大学, 广西隐伏金属矿产勘查重点实验室, 桂林 541004
桂林理工大学地球科学学院, 桂林 541004         miaobk@glut.edu.cn
谢兰芳         桂林理工大学, 广西隐伏金属矿产勘查重点实验室, 桂林 541004
桂林理工大学地球科学学院, 桂林 541004         
夏志鹏         桂林理工大学, 广西隐伏金属矿产勘查重点实验室, 桂林 541004
桂林理工大学地球科学学院, 桂林 541004         
基金项目：本文受国家自然科学基金项目(41173077)和广西隐伏金属矿产勘查重点实验室主任基金项目(13-A-01-02)联合资助.
摘要：
      月球陨石MIL05035岩石类型上属于普通辉石低钛玄武岩,粗粒辉长结构,无角砾化.主要矿物为辉石(60.2%)、斜长石(27.3%)和橄榄石(6.05%),次要矿物为石英(4.36%)、钛铁矿(1.25%)和陨硫铁(0.84%),含极少量富Ti、Fe尖晶石和磷灰石,广泛发育由钙铁辉石+铁橄榄石+石英组成的后成合晶三相集合体.辉石颗粒具有明显的化学成分不均匀性和出溶片晶,核部相对贫铁钙富镁(Fs30.2-60.8Wo14.2-35.0),边部富铁钙贫镁(Fs47.5-64.9Wo22.8-44.3).熔长石化斜长石具有微弱的成分环带,边部相对富碱金属元素(Ab9.3-12.3, Or0.31-1.03),核部则相反(Ab7.6-10.6, Or0.12-0.36),含有未熔长石化的残留斜长石.橄榄石具有粗晶橄榄石(Fa95.5-96.6)和后成合晶中细粒橄榄石(Fa88.9-93.5)两种产状.石英具有脉状、团块状和蠕虫状等产状:脉状石英大部分转变为二氧化硅玻璃,核部石英具有较宽的拉曼谱特征峰(448~502cm-1),证明其经历了冲击变质与退变质作用;团块状石英分布于粗粒橄榄石颗粒间或橄榄石与斜长石和辉石接触边界上,与斜长石构成充填结构;蠕虫状石英分布于细粒后成合晶中.粗粒辉石边部铁辉石和后成合晶中辉石成分的继承性、结构上的延续性、光学特征上的冲击暗化现象、与冲击熔脉结构上的相关性和后成合晶中发育与粗粒辉石方向几乎一致的解理等方面的证据,认为后成合晶可能由于铁辉石在冲击压力释放与温度降低后的退变质作用下分解形成.根据岩石矿物结构观察、成分分析和MELTS模拟表明该陨石母岩的岩浆演化过程可能为:母岩浆在温度降低后首先产生极少量钛铁尖晶石、其次是普通辉石和钙长石先后结晶;随着温度下降,贫钙铁普通辉石、铁钙铁辉石和铁普通辉石等在普通辉石边部大量结晶,钙长石边部分异结晶少量培长石或拉长石;随着温度继续下降,早期结晶的普通辉石析出易变辉石等出溶片晶,橄榄石在辉石和斜长石边部结晶;其后,钛铁矿和陨硫铁析出,石英沿橄榄石和钙长石等先结晶矿物裂隙充填.出露月表后强烈的冲击变质作用使斜长石几乎全部转变为熔长石、石英大部分转变为二氧化硅玻璃,并具有一系列面状变形,冲击熔脉发育,冲击变质程度至少为S5.本研究为月球的岩浆演化和冲击变质过程提供了重要证据.
英文摘要：
      Petrologically, the Lunar meteorite Miller Range (MIL) 05035 is low-Ti augite basalt, characterized by coarse gabbro texture and massive structure, non-breccia. It consists mainly of pyroxene (60.2%), plagioclase (27.3%), olivine (6.05%), quartz (4.36%), ilmenite (1.25%), troilite (0.84%), with minor spinel enriched Fe and Ti contents and apatite. Symplectites are composed of hedenbergite, fayalite and quartz. The pyroxene grains are distinctly heterogeneous with exsolution lamellae. The cores are enriched in MgO and depleted in CaO and FeO (Fs30.2-60.8Wo14.2-35.0) contents. By contrast, the rims are rich in CaO and FeO, and depleted in MgO contents. The maskelynites are weakly heterogeneous: the rims are relatively enriched in Na2O and K2O (Ab9.3-12.3, Or0.31-1.03) and the cores are inverse (Ab7.6-10.6, Or0.12-0.36). The olivine occurs as coarse grains (Fa95.5-96.6) and fine grains (Fa88.9-93.5) in symplectites. The quartz can also be divided into three types: veined, cloddy and helminthoid. The quartz vein is changed into glass of silica. The residual quartz has wide Raman spectra (448~502cm-1) implying that these quartz experienced strong shock metamorphism and retrogressive metamorphism; cloddy quartz locates in the boundary between olivine and plagioclase or olivine, which formed filling structure with plagioclase; helminthoid quartz distributes in the symplectite assemblages. The identical composition, continued structure, impact darken Phenomena, correlation with fusion vein and dentical cleavage trend indicate that symplectites are derived from pyroxene grains induced by shock retrogressive metamorphism. The integration of petrographic observation, mineral chemistry and MELTS modelling indicate that the magma evolution processes experienced following scenarios: when the temperature decreased, spinel crystallized from parent magma, augite and anorthite were followed; as the temperature fell down, pigeonite, ferriferous augite and hedenbergite were generated, the evolution of anorthite stopped or generated a bit of bytownites and labradorites. When the temperature continued decreasing, olivine crystallized from residual magma, followed by the ilmenite and troilite, quartz was enriched in Al and K intruded along the fractures between the augite, olivine and plagioclase grains. When the rock exposed on the surface of the moon, because of the shock metamorphism, the plagioclases were transformed into maskelynites, quartz partly changed into glass and presence of fusion veins, which indicate that MIL05035 experienced strong shock metamorphism, with the degree is at least S5. This study provides convincing evidence for the early lunar magma evolution and later shock metamorphism.

低调一点儿

好帖！欢人百花其放!但是，我怕都不听话的话，明天我就检不到异类陨石，特别是火星和月星！

小荷尖

我只知道石英只存在于地球这观点是错的，不含铁镍的就确定不是陨石也肯定是错的

洱海之源

怎么回事？没人发帖？

草原猎星人

没有确切的样品，，不好评判。