地质学家研究了早侏罗世(普林斯巴期)位于英国多塞 (IMAGE) Proceedings of the National Academy of Sciences Caption 地质学家研究了早侏罗世(普林斯巴期)位于英国多塞特的Belemnite Marl Member岩石群,泥岩的组成显示了与轨道变化相关的不同,这与来自威尔士的岩芯所显示的情况相似。 Credit 图片由Micha Ruhl提供。 Usage Restrictions None License Licensed content Disclaimer: AAAS and EurekAlert! are not responsible for the accuracy of news releases posted to EurekAlert! by contributing institutions or for the use of any information through the EurekAlert system.