Fission track dating of apatites
Fission track dating of apatites
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DOI：
10.1016/0012-821x(68)90072-1
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发表时间：
1968-07
影响因子：
5.3
通讯作者：
G. Wagner
中科院分区：
文献类型：
--
作者：
G. Wagner
首次对大量磷灰石进行了裂变径迹测年。在磷灰石中，如果使用油浸技术，很容易识别（0001）面上的裂变径迹。磷灰石中的裂变痕迹存活了100万年只有当温度不超过100°C时。对取自德国奥登瓦尔德不同类型岩石的磷灰石进行了研究。获得的裂变径迹年龄必须单独解释。火山岩中磷灰石的结晶年龄。与此相反，磷灰石年龄获得的基底岩石（花岗岩，花岗闪长岩，辉长岩）与奥登瓦尔德的隆升历史。
Fission track dating was applied to a large number of apatites for the first time. In apatite it is easy to identify fission tracks on the (0001) face if one uses the oil immersion technique. Fission tracks in apatite survive 1 m.y. only if the temperature does not exceed 100°C. Apatites taken from different types of rocks from the Odenwald (Germany) were studied. The fission track ages obtained have to be interpreted individually. The apatites taken from volcanic rocks yield crystallization ages. In contrast, apatite ages obtained on basement rocks (granites, granodiorites, gabbros) are related to the uplift history of the Odenwald.