Chen Huifang. 1991.Discovery of the old crystalline basement and komatiite on Hainan island.Geotectonica et Metallogenia,15(1) :62.

[1]陈惠芳.1991.海南岛前寒武纪结晶基底和科马提岩发现.大地构造与成矿学,15(1):62.

O'Neill says by looking at the water content and oxidation ratio of the komatiite samples they were able to discount the wet-melting theory.

奥尼尔说，通过观测科马堤岩样品量和氧化速度，他们以不用注重湿流体。

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接触带上，发育一条晚太古宙-古元古宙时期线性活动带。

Chen Huifang. 1991.Discovery of the old crystalline basement and komatiite on Hainan island.Geotectonica et Metallogenia,15(1) :62.

[1]陈惠芳.1991.海南岛前寒武纪结晶基底和科马提岩的发现.大地构造与成矿学,15(1):62.

O'Neill says by looking at the water content and oxidation ratio of the komatiite samples they were able to discount the wet-melting theory.

奥尼尔说，通科马堤岩样品的水含量和氧化速度，他们以不用注重湿流体理论了。

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.

在龙岗地块与间的接触上，发育了一条晚太古宙-古元古宙时期的线性活动。

Chen Huifang. 1991.Discovery of the old crystalline basement and komatiite on Hainan island.Geotectonica et Metallogenia,15(1) :62.

[1]陈惠芳.1991.海南岛前寒武纪结晶基底和科马提岩的发现.大地构造与成矿学,15(1):62.

O'Neill says by looking at the water content and oxidation ratio of the komatiite samples they were able to discount the wet-melting theory.

奥尼尔说，通过观测科马堤岩样品的水含量和氧化速度，他们以不用注重湿流体理论了。

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接触带上，发育了一条晚太古宙-古元古宙时期的线性活动带。

Chen Huifang. 1991.Discovery of the old crystalline basement and komatiite on Hainan island.Geotectonica et Metallogenia,15(1) :62.

[1]陈惠芳.1991.海南岛前寒武纪结晶基底和科马提岩发现.大地构造与成矿学,15(1):62.

O'Neill says by looking at the water content and oxidation ratio of the komatiite samples they were able to discount the wet-melting theory.

奥尼，过观测科马堤岩样品水含量和氧化速度，他们以不用注重湿流体理论了。

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触带上，发育了一条晚太古宙-古元古宙时期线性活动带。

Chen Huifang. 1991.Discovery of the old crystalline basement and komatiite on Hainan island.Geotectonica et Metallogenia,15(1) :62.

[1]惠芳.1991.海南岛前寒武纪结晶基底和科马提岩的发现.大地构造与成矿学,15(1):62.

O'Neill says by looking at the water content and oxidation ratio of the komatiite samples they were able to discount the wet-melting theory.

奥尼尔说，通过观测科马堤岩样品的水含量和氧化速度，他们以不用注重湿流体理论了。

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接触带上，发育了一条晚太古宙-古元古宙时期的线活动带。

Chen Huifang. 1991.Discovery of the old crystalline basement and komatiite on Hainan island.Geotectonica et Metallogenia,15(1) :62.

[1]陈惠.1991.岛前寒武纪结晶基底和科马提岩的发现.大地构造与成矿学,15(1):62.

O'Neill says by looking at the water content and oxidation ratio of the komatiite samples they were able to discount the wet-melting theory.

奥尼尔说，通过观测科马堤岩样品的水含量和氧化速度，他们以不用注重湿流体理论了。

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接触带，发育了一条晚太古宙-古元古宙时期的线性活动带。

Chen Huifang. 1991.Discovery of the old crystalline basement and komatiite on Hainan island.Geotectonica et Metallogenia,15(1) :62.

[1]陈惠芳.1991.海南岛前寒武纪结晶基底和科马的发现.大地构造与成矿学,15(1):62.

O'Neill says by looking at the water content and oxidation ratio of the komatiite samples they were able to discount the wet-melting theory.

奥尼尔说，通过观测科马堤样品的水含量和氧化速度，他们以不用注重湿流体理论了。

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接触带上，发育了一条晚太古宙-古元古宙时期的线性活动带。

Chen Huifang. 1991.Discovery of the old crystalline basement and komatiite on Hainan island.Geotectonica et Metallogenia,15(1) :62.

[1]陈惠芳.1991.海南岛前寒武纪结晶基底和科马提岩的.地构造与成矿学,15(1):62.

O'Neill says by looking at the water content and oxidation ratio of the komatiite samples they were able to discount the wet-melting theory.

奥尼尔说，通过观测科马堤岩样品的水含量和氧化速度，他们以不用注重湿流体理论了。

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接触带上，育了一条晚-元时期的线性活动带。

Chen Huifang. 1991.Discovery of the old crystalline basement and komatiite on Hainan island.Geotectonica et Metallogenia,15(1) :62.

[1]惠芳.1991.海南岛前寒武纪结晶基底和科马提岩的发现.大地构造与成矿学,15(1):62.

O'Neill says by looking at the water content and oxidation ratio of the komatiite samples they were able to discount the wet-melting theory.

奥尼尔说，通过观测科马堤岩样品的水含量和氧化速度，他们以不用注重湿流体理论了。

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接触带上，发育了一条晚太古宙-古元古宙时期的线活动带。