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.

东加那利群是内围层的一个例子已完全确实，它在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.

东群岛地块是内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，发育了条晚太古宙-古元古宙时期的线活动带。

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

东加那利群岛内围层的一个例子已完全确实，它在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.

龙岗地块与北带之间的触带上，发育了一条晚太-元时期的线性活动带。