The sunstone theory was first proposed in 1966 by the Danish archaeologist Thorkild Ramskou.

关（使用）日长石（导航的）理论，最丹麦考古学家托基尔德·拉姆斯库1966年提出。

Cumulate plagioclase appears abruptly at the base of the F unit, which rests on an erosional disconformity .

堆积的斜长石在位侵蚀假整合之上的F单元的基底突然出现。

The albite component increases while anorthic component decreases in detrital plagioclase.The plagioclase turned into an end - member component of albite.

斜长石碎屑中钠长石组逐渐增多，钙长石组逐渐减少，最终形纯钠端元的钠长石。

Therefore, the albitization of plagioclase is shown in the early stage of diagenesis and albitization of potash feldspar appears only in the late stage of diagenesis.

因此，斜长石的钠长石化可见早期，而钾长石的钠长石化只发生晚期。

Depending on the chemical composition the structural parameters of the melilite vary in the range between gehlenite and mernite.Melilitic separation and melilite as a primary phase are very rare.

黄长石的结构参数，按其化学在钙铝黄长石和镁黄长石之间变化，黄长石作为原始矿物相在碱性矿渣中比较罕见。

The sunstone theory was first proposed in 1966 by the Danish archaeologist Thorkild Ramskou.

关于（使用）日长石（导航的）理论，最初是由丹麦考古学家托基尔德·拉姆斯库于1966年提。

Cumulate plagioclase appears abruptly at the base of the F unit, which rests on an erosional disconformity .

的斜长石在位于侵蚀假整合之上的F单元的基底突然现。

The albite component increases while anorthic component decreases in detrital plagioclase.The plagioclase turned into an end - member component of albite.

斜长石碎屑中钠长石组逐渐增多，钙长石组逐渐减少，最终形成纯钠端元的钠长石。

Therefore, the albitization of plagioclase is shown in the early stage of diagenesis and albitization of potash feldspar appears only in the late stage of diagenesis.

因此，斜长石的钠长石于成岩早期，而钾长石的钠长石只发生于成岩晚期。

Depending on the chemical composition the structural parameters of the melilite vary in the range between gehlenite and mernite.Melilitic separation and melilite as a primary phase are very rare.

黄长石的结构参数，按其学成是在钙铝黄长石和镁黄长石之间变，黄长石作为原始矿物相在碱性矿渣中比较罕。

The sunstone theory was first proposed in 1966 by the Danish archaeologist Thorkild Ramskou.

于（使用）日长石（导航的）理论，最初是由丹麦考古家托基尔德·拉姆斯于1966年提出。

Cumulate plagioclase appears abruptly at the base of the F unit, which rests on an erosional disconformity .

堆积的斜长石在位于侵蚀假整合之上的F单元的基底突然出现。

The albite component increases while anorthic component decreases in detrital plagioclase.The plagioclase turned into an end - member component of albite.

斜长石碎屑中钠长石组逐渐增多，钙长石组逐渐减少，最终形纯钠端元的钠长石。

Therefore, the albitization of plagioclase is shown in the early stage of diagenesis and albitization of potash feldspar appears only in the late stage of diagenesis.

因此，斜长石的钠长石可见于岩早期，而钾长石的钠长石只发生于岩晚期。

Depending on the chemical composition the structural parameters of the melilite vary in the range between gehlenite and mernite.Melilitic separation and melilite as a primary phase are very rare.

黄长石的结构参数，按其是在钙铝黄长石和镁黄长石之间变，黄长石作为原始矿物相在碱性矿渣中比较罕见。

The sunstone theory was first proposed in 1966 by the Danish archaeologist Thorkild Ramskou.

关于（使用）日（航）理论，最初是由丹麦考古学家托基尔德·拉姆斯库于1966年提出。

Cumulate plagioclase appears abruptly at the base of the F unit, which rests on an erosional disconformity .

堆积斜在位于侵蚀假整合之上F单元基底突然出现。

The albite component increases while anorthic component decreases in detrital plagioclase.The plagioclase turned into an end - member component of albite.

斜碎屑中钠组逐渐增多，钙组逐渐减少，最终形成纯钠端元钠。

Therefore, the albitization of plagioclase is shown in the early stage of diagenesis and albitization of potash feldspar appears only in the late stage of diagenesis.

因此，斜钠化可见于成岩早期，而钾钠化只发生于成岩晚期。

Depending on the chemical composition the structural parameters of the melilite vary in the range between gehlenite and mernite.Melilitic separation and melilite as a primary phase are very rare.

黄参数，按其化学成是在钙铝黄和镁黄之间变化，黄作为原始矿物相在碱性矿渣中比较罕见。

The sunstone theory was first proposed in 1966 by the Danish archaeologist Thorkild Ramskou.

关于（使用）日长石（导航的）理论，最初是由丹麦考古家托基尔德·拉姆斯于1966年提出。

Cumulate plagioclase appears abruptly at the base of the F unit, which rests on an erosional disconformity .

堆积的斜长石在位于侵蚀假整合之上的F单元的基底突然出现。

The albite component increases while anorthic component decreases in detrital plagioclase.The plagioclase turned into an end - member component of albite.

斜长石碎屑中钠长石组逐渐增多，钙长石组逐渐减少，最终形纯钠端元的钠长石。

Therefore, the albitization of plagioclase is shown in the early stage of diagenesis and albitization of potash feldspar appears only in the late stage of diagenesis.

因此，斜长石的钠长石化可见于岩早期，而钾长石的钠长石化只发生于岩晚期。

Depending on the chemical composition the structural parameters of the melilite vary in the range between gehlenite and mernite.Melilitic separation and melilite as a primary phase are very rare.

黄长石的结构参数，按其化是在钙铝黄长石和镁黄长石之间变化，黄长石作为原始矿物相在碱性矿渣中比较罕见。

The sunstone theory was first proposed in 1966 by the Danish archaeologist Thorkild Ramskou.

关于（使用）日（导航的）理论，最初是由丹麦考古基尔德·拉姆斯库于1966年提出。

Cumulate plagioclase appears abruptly at the base of the F unit, which rests on an erosional disconformity .

堆积的斜在位于侵蚀假整合之上的F单元的基底突然出现。

The albite component increases while anorthic component decreases in detrital plagioclase.The plagioclase turned into an end - member component of albite.

斜碎屑中组逐渐增多，钙组逐渐减少，最终形成纯端元的。

Therefore, the albitization of plagioclase is shown in the early stage of diagenesis and albitization of potash feldspar appears only in the late stage of diagenesis.

因此，斜的化可见于成岩早期，而钾的化只发生于成岩晚期。

Depending on the chemical composition the structural parameters of the melilite vary in the range between gehlenite and mernite.Melilitic separation and melilite as a primary phase are very rare.

黄的结构参数，按其化成是在钙铝黄和镁黄之间变化，黄作为原始矿物相在碱性矿渣中比较罕见。

The sunstone theory was first proposed in 1966 by the Danish archaeologist Thorkild Ramskou.

关于（使用）日（导航）理论，最初是由丹麦考古学家托基尔德·拉姆斯库于1966年提出。

Cumulate plagioclase appears abruptly at the base of the F unit, which rests on an erosional disconformity .

堆积斜于侵蚀假整合之上F单元基底突然出现。

The albite component increases while anorthic component decreases in detrital plagioclase.The plagioclase turned into an end - member component of albite.

斜碎屑中钠组逐渐增多，钙组逐渐减少，最终形成纯钠端元钠。

Therefore, the albitization of plagioclase is shown in the early stage of diagenesis and albitization of potash feldspar appears only in the late stage of diagenesis.

因此，斜钠化可见于成岩早期，而钾钠化只发生于成岩晚期。

Depending on the chemical composition the structural parameters of the melilite vary in the range between gehlenite and mernite.Melilitic separation and melilite as a primary phase are very rare.

黄结构参数，按其化学成是钙铝黄和镁黄之间变化，黄作为原始矿物相碱性矿渣中比较罕见。

The sunstone theory was first proposed in 1966 by the Danish archaeologist Thorkild Ramskou.

关于（使用）日长石（导航的）理论，由丹麦考古学家托基尔德·拉姆斯库于1966年提出。

Cumulate plagioclase appears abruptly at the base of the F unit, which rests on an erosional disconformity .

堆积的斜长石在位于侵蚀假整合之上的F单元的基底突然出现。

The albite component increases while anorthic component decreases in detrital plagioclase.The plagioclase turned into an end - member component of albite.

斜长石碎屑中钠长石组逐渐增多，钙长石组逐渐减少，终形纯钠端元的钠长石。

Therefore, the albitization of plagioclase is shown in the early stage of diagenesis and albitization of potash feldspar appears only in the late stage of diagenesis.

因此，斜长石的钠长石化可见于早期，而钾长石的钠长石化只发生于期。

Depending on the chemical composition the structural parameters of the melilite vary in the range between gehlenite and mernite.Melilitic separation and melilite as a primary phase are very rare.

黄长石的结构参数，按其化学在钙铝黄长石和镁黄长石之间变化，黄长石作为原始矿物相在碱性矿渣中比较罕见。

The sunstone theory was first proposed in 1966 by the Danish archaeologist Thorkild Ramskou.

关于（使用）日长石（导航的）理论，初是由丹麦考古学家托尔德·拉姆斯库于1966年提出。

Cumulate plagioclase appears abruptly at the base of the F unit, which rests on an erosional disconformity .

堆积的斜长石在位于侵蚀假整合之上的F单元的然出现。

The albite component increases while anorthic component decreases in detrital plagioclase.The plagioclase turned into an end - member component of albite.

斜长石碎屑中钠长石组逐渐增多，钙长石组逐渐减少，成纯钠端元的钠长石。

Therefore, the albitization of plagioclase is shown in the early stage of diagenesis and albitization of potash feldspar appears only in the late stage of diagenesis.

因此，斜长石的钠长石化可见于成岩早期，而钾长石的钠长石化只发生于成岩晚期。

Depending on the chemical composition the structural parameters of the melilite vary in the range between gehlenite and mernite.Melilitic separation and melilite as a primary phase are very rare.

黄长石的结构参数，按其化学成是在钙铝黄长石和镁黄长石之间变化，黄长石作为原始矿物相在碱性矿渣中比较罕见。

The sunstone theory was first proposed in 1966 by the Danish archaeologist Thorkild Ramskou.

关于（使用）日长石（导航的）理论，最初是由丹麦考古学家托基尔德·拉姆斯库于1966年提出。

Cumulate plagioclase appears abruptly at the base of the F unit, which rests on an erosional disconformity .

堆积的斜长石在位于侵蚀假整合之上的F单元的基底突然出现。

The albite component increases while anorthic component decreases in detrital plagioclase.The plagioclase turned into an end - member component of albite.

斜长石碎屑中钠长石组逐渐增多，长石组逐渐减少，最终形成纯钠端元的钠长石。

Therefore, the albitization of plagioclase is shown in the early stage of diagenesis and albitization of potash feldspar appears only in the late stage of diagenesis.

因此，斜长石的钠长石化可见于成岩早期，而钾长石的钠长石化只发生于成岩晚期。

Depending on the chemical composition the structural parameters of the melilite vary in the range between gehlenite and mernite.Melilitic separation and melilite as a primary phase are very rare.

长石的结构参数，按其化学成是在长石和镁长石之间变化，长石作为原始矿物相在碱性矿渣中比较罕见。