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首页> 外文期刊>The Open Geology Journal >Mapping Absolute Migration of the Indian Triple Junction Since 75 Ma and Implication for its Evolution
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Mapping Absolute Migration of the Indian Triple Junction Since 75 Ma and Implication for its Evolution

机译:映射自75 Ma以来印度三重交界处的绝对迁移及其演变的意义

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The absolute migration of the Indian Triple Junction (ITJ) or also known as the Rodriguez Triple Junction (RTJ) has been mapped using published data. The ITJ is made of the Southwest Indian Ridge (SWIR), the Central Indian Ridge (CIR) and the Southeast Indian Ridge (SEIR). The traces of the ITJ on the three plates (Africa, Antarctica, and Australia) were reconstructed to their former positions in the hotspot reference frame to map its absolute migration for the past 75 million years. The ITJ migrated northeasterly at a speed of 10 cm/yr at 70 Ma that declined gradually to 2.6 cm/yr at 43 Ma and thereafter remaining almost constant about 3.6-3.8 cm/yr, in a fairly straight trajectory suggesting a stable configuration of the ITJ since its formation. Because the most stable configuration known is the Ridge-Ridge-Ridge (RRR) triple junction, it is suggested that the configuration of the ITJ has been largely an RRR triple junction since its formation.
机译:印度三重连接点(ITJ)或也称为Rodriguez三重连接点(RTJ)的绝对迁移已使用已发布的数据进行了映射。 ITJ由西南印第安岭(SWIR),中印第安岭(CIR)和东南印第安岭(SEIR)组成。将ITJ在三个板块(非洲,南极洲和澳大利亚)上的迹线重建到热点参考系中的先前位置,以绘制其在过去7,500万年的绝对迁移图。 ITJ在70 Ma处以每年10 cm / yr的速度向东北迁移,在43 Ma处逐渐下降至2.6 cm / yr,此后几乎保持恒定,约为3.6-3.8 cm / yr,这是一条相当笔直的轨迹,表明该构造稳定。 ITJ自成立以来。因为已知的最稳定的配置是Ridge-Ridge-Ridge(RRR)三重结,所以建议ITJ的结构自形成以来就主要是一个RRR三重结。

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