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TECTONIC COMPLEXITIES IN SOUTH FIJI MARGINAL BASIN

机译:斐济南部边缘盆地的构造复杂性

摘要

Two magnetic lineation patterns occur in the South Fiji marginal basin. North-south lineation, which are parallel to the Lau-Colville ridge, are identified as anomalies 8 through 12 (29-35 m.y. B.P.). The inferred age of the basin increases eastward to the ridge. These identifications are consistent with DSDP drilling results and suggest that at least part of the basin formed in the Oligocene. These results, together with our previous study of magnetic lineations in the Shikoku basin south of Japan, also imply that the mechanism of crustal accretion in marginal basins is similar to that at mid-ocean ridges. Unidentified east-west-trending lineations west of the northsouth pattern suggest a complicated tectonic history for the South Fiji basin. It seems that the evolution of the basin involved more than just one simple two-limb spreading system. © 1975.
机译:斐济南部边缘盆地有两种磁性线型。平行于Lau-Colville脊的南北走向被确定为8到12异常(B.P. 29-35 m.y.)。盆地的推断年龄向东延伸至山脊。这些识别结果与DSDP钻探结果一致,表明至少有一部分盆地是在渐新世形成的。这些结果,再加上我们先前对日本南部四国盆地磁线学的研究,也暗示边缘盆地的地壳增生机制与洋中脊相似。南北格局以西的不明的东西向趋势线表明,斐济南部盆地的构造历史复杂。盆地的演化似乎不仅仅涉及一种简单的两肢扩散系统。 ©1975。

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    WEISSEL J; WATTS A;

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  • 年度 1975
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