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.

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.

东加那利群岛块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.

在块与北带之间的触带上，发育了一古宙-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.

在龙岗地块与北的触，育了一条晚太古宙-古元古宙时期的线性活动。

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

东加那利群岛块是内围层的一个例子已完全确实，它在与相邻的大陆有关。

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上，发育了一条晚太古宙-古元古宙线性活动带。

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

东加那利群岛是内围层的个例子已完全确实，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.

在龙与北带之间的触带上，发育了太古宙-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，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。