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The southern part of the Outer Zone of Southwest Japan including the Kii peninsula belongs to the tectonic 'shadow zone', where fewer conspicuous active faults and less Quaternary sediments develop than in the Nankai subduction zone and Inner Zone of Southwest Japan. In order to study the paleostress sequence of the Kii peninsula, we analyzed fault-slip data and tension gashes at pilot sites of Early-Middle Miocene forearc sediments and Late Cretaceous accretionary complex. According to the results, six faulting events are reconstructed in sequence: (i) east-west extension (normal faulting); (ii) east-west compression and north-south extension (strike-slip faulting); (iii) NNW-SSE compression and ENE-WSW extension (strike-slip faulting); (iv) northeast-southwest compression and northwest-southeast extension (strike-slip faulting); (v) WNW-ESE compression (strike-slip or reverse faulting); and (vi) NNE-SSW extension. The north-south to NNW-SSE trending dyke swarm of Middle Miocene age in the Kii peninsula is thought to be related to Event 3, implying that Event 3 was active at least during the Middle Miocene. Because Event 6 is recognized solely at a site, the overall latest faulting event seems to be Event 5. Assuming that the compression results from the motion of the crust or plate, the compression direction of Event 5 is in good accordance with the present-day WNW crustal velocity vectors of the Kii peninsula. The stress trajectory map of Southeast Korea and Southwest Japan reveals that the current compression directions of the Kii peninsula correspond to the combinatory stress fields of the Himalayan and Philippine Sea tectonic domains. [ABSTRACT FROM AUTHOR]