黄河山陕峡谷保德-克虎段高阶地砾石层的初步研究

野外考察发现山西黑峪口地区存在七级阶地序列,其中上覆红粘土的T6、T7阶地为晚第三纪阶地.对该区阶地上砾石的岩性和粒径进行了研究,岩性对比表明,T6、T7阶地上砾石的岩性与黄河低阶地上砾石的岩性相似,而与东西向的蔚汾河阶地岩性差别较大;上下游之间对比发现,灰岩砾石岩性由保德地区占主导地位到克虎地区退居次要地位,灰岩砾石的粒径也从上游向下游变小,说明该区晚第三纪阶地并非东西向河流形成的,而是古黄河或古南北向水系的产物.T7阶地上覆盖厚度70m以上的粉、细砂层和晚第三纪红土层,磁性地层研究表明,该层的底部时代在6.8Ma左右,T6阶地上覆红粘土的底部年龄在3.3Ma左右,山陕峡谷由北向南流的古河流在6.8Ma之前已经形成,T6阶地的形成时代与青藏运动A幕相对应.青藏运动A幕以来河流在该区下切了160m,平均下切速率约为青藏运动A幕以前平均下切速率的5倍以上.     

New paleomagnetic results from the Yangzhuang Formation of the Jixian System,North China,and tectonic implications

A paleomagnetic study was carried out on the Yangzhuang Formation （-1350 Ma） of the Jixian System in the North China Block （NCB）. Detailed stepwise thermal demagnetization isolated two components. The soft component （component A） was interpreted as a remagnetization in the recent geomagnetic field. The hard component （component B） with higher unblocking-temperatures was carried by hematite. Its site-mean direction is D/I = 77.6°/-24.3°κ= 5.4, α 95 = 18.3°, N = 15 sites） before, and D/I = 72.2°/11.5° （ κ=24.6, α95 = 7.9°） after tilt correction. It passes a fold test（Mesozoic folding） at 99% confidence level and reversal test at 95% confidence level. The corresponding pole locates at 17.3°N, 214.5°E （dp = 4.1°, dm= 8.0°）. A best fit of paleomagnetic poles from the NCB, Baltica, Siberia and the apparent polar wander path for Laurentia suggests a long-lived connection between these paleo-continents between -1800and 1350 Ma.     

华北地块沁水盆地下三叠统刘家沟组古地磁倾角浅化研究

对华北地块沁水盆地下三叠统刘家沟组红层样品进行系统的岩石磁学、磁组构和古地磁学研究, 并用E/I (elongation/inclination)方法对其进行磁倾角浅化的识别与校正, 获得刘家沟组红层磁倾角浅化因子f = 0.6。岩石磁学结果显示, 刘家沟组红层的主要载磁矿物是赤铁矿及磁铁矿, 其磁组构具有典型的静水沉积特征。经地层校正后, 15个采样点特征剩磁分量的平均方向为D_s=318.8°, I_s=30.9°(α₉₅= 6.9°), 对应的古地磁极为49.3°N, 5.5°E (A₉₅=6.7°), 磁倾角浅化校正后的古地磁极为53.5°N, 18.0°E。对包括本文数据在内的高质量的华北早三叠世古地磁极数据(Q≥4)进行平均, 得到校正前的古地磁极为55.3°N, 357.1°E (A₉₅=5.5°), 校正后的古地磁极为60.8°N, 13.4°E (A₉₅=5.8°)。经过古地磁倾角浅化校正, 华北地块早三叠世的古纬度有约10°的明显提高, 指示其东部早三叠世时与华南地块之间可能存在一定的纬度差, 但是该纬度差很可能并不代表华北地块东部早三叠世时与华南地块尚未对接, 而是指示华南地块下三叠统灰岩同样存在显著的磁倾角浅化现象。     

泥盆纪华南板块古地理的位置及其漂移

华南板块在泥盆纪位于古赤道附近,早—中泥盆世之交,广西那艺古纬度为 0°36',泥盆纪—石炭纪之交贵州睦化地区古纬度为4°10'10″,赤道附近温湿的气候使华南板块上各种生物,无脊椎动物,脊椎动物,植物高度繁盛,发育,都有很高的分异度。泥盆纪时期华南板块向北缓慢移动,移动速率为0.22 ～0.26cm/a。其原因可能与特提斯洋的活动有关。     

保山地块晚石炭世玄武岩古地磁研究及构造归属的新认识

通过对保山地块晚石炭世玄武岩东、西带代表性剖面的古地磁研究,认为东、西带玄武岩古地磁测量数据的差异是因取样点的古构造古地理背景不同造成的。结合两带玄武岩浆喷溢时所处的构造背景和古地形特征,作者提出西带玄武岩的古地磁数据能较准确地反映地块当时应位于南半球低纬(15.6°)区,而不是过去认为的高纬区。保山地块不是冈瓦纳大陆的一部分,它与扬子地块间不存在古特提斯大洋,而可能是毗邻扬子地块的一个小地块。     

Tectonic rotation in the western South-Dabashan orogenic belt in late Mesozoic

A paleomagnetic study was carried out on Early-Middle Jurassic sediments in the Zhenba area, the western South-dabashan orogenic belt. Stepwise thermal demagnetization isolated the characteristic high temperature component (HTC) (D=37.1°, I=46.1°, α95=10.1°), which passed the fold test. By comparing the corresponding pole of HTC (57.6°N, 196.6°E, A95=9.9°) with coeval reference poles for the Sichuan basin, we detected a 26.5°±9.0° clockwise rotation of the study area relative to the stable Sichuan basin. We...     

Paleomagnetism of early Paleozoic volcanic rocks from the Beishan area,Gansu of northwest China: Preliminary insight into early Paleozoic kinemics of the Beishan terrane

We report rock magnetic and paleomagnetic results for Middle Silurian Gongpoquan and Middle Ordovician Huaniushan volcanic samples collected from the Mazongshan and Hongliuyuan areas of Gansu Province, northwest China. The resultsindicate that the main magnetic mineral of the Gongpoquan and Huaniushan volcanic rock is magnetite, and it may remain characteristic remanent magnetization acquired at the time of formation of the rocks. However, with the exception of samples from site go20, most of Middle Ordovician Huaniushan volcanic samples have a very weak nature remanent magnetization, and generally show an erratic demagnetization behavior, which does not allow isolation of characteristic remanent magnetizations from these samples. Comparison of paleomagnetic results obtained from the Beishan area of Gansu with Paleozoic apparent polar wander paths for Tarimand Siberia suggests that the Beishan tarrane, the southern part of the Beishanarea of Gansu beyond the Mingshui-Shipanjin-Xiaohuang- shan zone, and adjacent Tarim block and Siberia plate could not have been connected in their present configuration by the Middle Silurian time. On the other hand, we infer that the early Paleozoic Mingshui-Shipanjin-Xiaohuangshan oceanic basin may open from west to east during period from the Ordovician to Silurian, and the post-Middle Silurian closing of this oceanic basin may result from a progressed eastward scissor-like rotation.