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华南石炭纪岩关-大塘界线期牙形石地层分带 总被引：4，自引：0，他引：4
系统采集不同沉积相区和连续沉积的剖面，即浅海台地相广西柳江龙殿山剖面、台缘缓坡相云南施甸鱼硐剖面和台内盆地相广西柳州碰冲剖面，运用数理统计方法，研究了华南岩关一大塘界线过渡期牙形石的产出丰度和相分布，在恢复生物演化序列的基础上，对各剖面首先详细分带，再进一步综合成系统的5个牙形石带，即Gnathodus typicus—G．cuneiformis带、Gnathodus typicus—Protognathodus cordiformis带、Scaliognathus anchoralis—Gnathodus pseu-dosemiglaber带、Gnathodus praebilineatus带和Paragnathodus horrtopunctatus带。以生物系统发生为标准，严格限定各带的界线，并与北美、西欧同期地层进行精确对比，为建立杜内阶一维宪阶界线的全球层型(GSSP)提供可靠依据。 相似文献
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目的:探讨双能CT在膝关节前交叉韧带(ACL)损伤中的应用可行性。方法:30例膝关节外伤患者行双能CT和MR检查,观察软组织CT图像、双能CT肌腱伪彩(DETC)图像和MR图像上ACL。以MR图像为参考标准,评估双能CT图像诊断ACL损伤的预测值。结果:MR图像、软组织CT图像、联合软组织CT图像和DETC图像诊断明确的ACL损伤的例数分别为23、11和20。软组织CT图像诊断ACL损伤的敏感度、特异度、阳性预测值、阴性预测值及准确度分别为47.8%、100.0%、100.0%、36.8%和60.0%;联合软组织CT图像和DETC图像诊断ACL损伤的各预测值分别为82.6%、85.7%、95.0%、60.0%和83.3%。与软组织CT图像相比,联合软组织CT图像和DETC图像诊断ACL损伤的敏感度和准确度均有明显增加(敏感度和准确度相应的χ2值分别为6.133和4.022,P值均<0.05)。结论:联合双能CT的软组织CT图像和DETC图像可诊断ACL损伤,并具有较高的预测值。 相似文献
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A deep-level crustal section of the Cretaceous Kohistan arc is exposed in the northern part of the Jijal complex. The occurrence of mafic to ultramafic granulite-facies rocks exhibits the nature and metamorphic evolution of the lower crust. Mafic granulites are divided into two rock types: two-pyroxene granulite (orthopyroxene+clinopyroxene+plagioclase±quartz [1]); and garnet–clinopyroxene granulite (garnet+clinopyroxene+plagioclase+quartz [2]). Two-pyroxene granulite occurs in the northeastern part of the Jijal complex as a relict host rock of garnet–clinopyroxene granulite, where the orthopyroxene-rich host is transected by elongated patches and bands of garnet–clinopyroxene granulite. Garnet–clinopyroxene granulite, together with two-pyroxene granulite, has been partly replaced by amphibolite (hornblende±garnet+plagioclase+quartz [3]). The garnet-bearing assemblage [2] is expressed by a compression–dehydration reaction: hornblende+orthopyroxene+plagioclase=garnet+clinopyroxene+quartz+H2O↑. Subsequent amphibolitization to form the assemblage [3] is expressed by two hydration reactions: garnet+clinopyroxene+plagioclase+H2O=hornblende+quartz and plagioclase+hornblende+H2O=zoisite+chlorite+quartz. The mafic granulites include pod- and lens-shaped bodies of ultramafic granulites which consist of garnet hornblendite (garnet+hornblende+clinopyroxene [4]) associated with garnet clinopyroxenite, garnetite, and hornblendite. Field relation and comparisons in modal–chemical compositions between the mafic and ultramafic granulites indicate that the ultramafic granulites were originally intrusive rocks which dissected the protoliths of the mafic granulites and then have been metamorphosed simultaneously with the formation of garnet–clinopyroxene granulite. The results combined with isotopic ages reported elsewhere give the following tectonic constraints: (1) crustal thickening through the development of the Kohistan arc and the subsequent Kohistan–Asia collision caused the high-pressure granulite-facies metamorphism in the Jijal complex; (2) local amphibolitization of the mafic granulites occurred after the collision. 相似文献
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