The East Canary Islands block is an example of an island inlier with a morphologically well defined relation to its adjacent continent.

东加那利群岛是内围层的个例子已完全确实，它在形上相邻的大陆有关。

To date, komatiites with spinifex textures have not been found in the supracrustal rocks, but rock sequences similar to greenstones metamorphosed up to upper amphibolite facies are often observed.

在龙岗北带之间的触带上，发育晚太古宙-古元古宙时期的线性活动带。

The East Canary Islands block is an example of an island inlier with a morphologically well defined relation to its adjacent continent.

东加那利群岛地块是内围层一个例子已完全确实，它在地形上与相陆有关。

To date, komatiites with spinifex textures have not been found in the supracrustal rocks, but rock sequences similar to greenstones metamorphosed up to upper amphibolite facies are often observed.

在龙岗地块与北带之间触带上，发育了一条晚太-元期线性活动带。

The East Canary Islands block is an example of an island inlier with a morphologically well defined relation to its adjacent continent.

东加那利群岛地块是内围层的一个例子已完全确实，它地形上与相邻的大陆有。

To date, komatiites with spinifex textures have not been found in the supracrustal rocks, but rock sequences similar to greenstones metamorphosed up to upper amphibolite facies are often observed.

岗地块与北带之间的触带上，发育了一条晚-元时期的线性活动带。

The East Canary Islands block is an example of an island inlier with a morphologically well defined relation to its adjacent continent.

东加那利群岛地块是内围层一个例子已完全确实，它在地相邻大陆有关。

To date, komatiites with spinifex textures have not been found in the supracrustal rocks, but rock sequences similar to greenstones metamorphosed up to upper amphibolite facies are often observed.

在龙岗地块北带之间触带，发育了一条晚太古宙-古元古宙时期活动带。

The East Canary Islands block is an example of an island inlier with a morphologically well defined relation to its adjacent continent.

东加那利群岛地块是内围层一个例子已完全确实，它在地形上与大陆有关。

To date, komatiites with spinifex textures have not been found in the supracrustal rocks, but rock sequences similar to greenstones metamorphosed up to upper amphibolite facies are often observed.

在龙岗地块与北带之间触带上，发育了一条晚太古-古元古线性活动带。

The East Canary Islands block is an example of an island inlier with a morphologically well defined relation to its adjacent continent.

东加那利群岛地块是内围层的一个全确实，它在地形与相邻的大陆有关。

To date, komatiites with spinifex textures have not been found in the supracrustal rocks, but rock sequences similar to greenstones metamorphosed up to upper amphibolite facies are often observed.

在龙岗地块与北带之间的触带，发育了一条晚太古宙-古元古宙时期的线性活动带。

The East Canary Islands block is an example of an island inlier with a morphologically well defined relation to its adjacent continent.

东加那利群岛地块是内围层的一个子已完全确实，它在地形上与相邻的大陆有关。

To date, komatiites with spinifex textures have not been found in the supracrustal rocks, but rock sequences similar to greenstones metamorphosed up to upper amphibolite facies are often observed.

在龙岗地块与北带之间的触带上，发育了一条晚太古宙-古元古宙时期的线性活动带。

The East Canary Islands block is an example of an island inlier with a morphologically well defined relation to its adjacent continent.

东加那利群岛地块是围层的一个例子已完全确实，它在地形上与相邻的大陆有关。

To date, komatiites with spinifex textures have not been found in the supracrustal rocks, but rock sequences similar to greenstones metamorphosed up to upper amphibolite facies are often observed.

在龙岗地块与北带之间的触带上，发育了一条晚太古宙-古元古宙时期的线性活动带。

The East Canary Islands block is an example of an island inlier with a morphologically well defined relation to its adjacent continent.

东加那利群岛地块是内围层的一个全确实，它在地形与相邻的大陆有关。

To date, komatiites with spinifex textures have not been found in the supracrustal rocks, but rock sequences similar to greenstones metamorphosed up to upper amphibolite facies are often observed.

在龙岗地块与北带之间的触带，发育了一条晚太古宙-古元古宙时期的线性活动带。