The extrusive rock unit includes basalt, andesite, boninite and albitite as well as breccia and tuff.

喷出岩单元不仅仅由玄武岩组成，还包括安山岩、玻安岩、钠长岩以及角砾岩、凝灰岩等。

The first rock is mainly andesite clinkering agglomerate, andesite breccia, dacite breccia, rhyolite breccia and rhyolite clinkering tuff.

正常火山碎屑岩亚类岩石类型主要为安山集块岩,安山、英安及火山角砾岩以及凝灰岩。

A new image shows possible "megabreccia" along the center of Mars's Coprates Chasma, a major trough in the Valles Marineris canyon system.

一种新的图像显示“巨形角砾岩”可能临近火星科普雷茨峡谷的中心，主要穿过瓦勒斯马里纳里斯峡谷山系。

Orebodies in sedirmentary rock hosted Au deposits are discrete hypogene and epigenetic masses usually hosted in a fault zone, breccia mass, or lithologic bed or unit.

沉积岩金矿床的矿体是一些不连续的内生或后生地体,通常赋存于断裂带、角砾岩体或岩层(岩性单位)中。

The extrusive rock unit includes basalt, andesite, boninite and albitite as well as breccia and tuff.

喷出岩单元不仅仅由玄武岩组成，还包括安山岩、玻安岩、钠长岩以及角砾岩、凝灰岩等。

The first rock is mainly andesite clinkering agglomerate, andesite breccia, dacite breccia, rhyolite breccia and rhyolite clinkering tuff.

正常火山碎屑岩亚岩主要为安山质熔结集块岩,安山质、英安质及纹质火山角砾岩以及纹质熔结凝灰岩。

A new image shows possible "megabreccia" along the center of Mars's Coprates Chasma, a major trough in the Valles Marineris canyon system.

一图像显示“巨形角砾岩”可能临近火星科普雷茨峡谷中心，主要穿过瓦勒斯马里纳里斯峡谷山系。

Orebodies in sedirmentary rock hosted Au deposits are discrete hypogene and epigenetic masses usually hosted in a fault zone, breccia mass, or lithologic bed or unit.

沉积岩金矿床矿体是一些不连续内生或后生地质体,通常赋存于断裂带、角砾岩体或岩层(岩性单位)中。

The extrusive rock unit includes basalt, andesite, boninite and albitite as well as breccia and tuff.

喷出单元不仅仅由玄武组成，还包括山、、钠长以及角砾、凝灰等。

The first rock is mainly andesite clinkering agglomerate, andesite breccia, dacite breccia, rhyolite breccia and rhyolite clinkering tuff.

正常火山碎屑亚类石类型要为山质熔结集块,山质、英质及纹质火山角砾以及纹质熔结凝灰。

A new image shows possible "megabreccia" along the center of Mars's Coprates Chasma, a major trough in the Valles Marineris canyon system.

一种新的图像显示“巨形角砾”可能临近火星科普雷茨峡谷的，要穿过瓦勒斯马里纳里斯峡谷山系。

Orebodies in sedirmentary rock hosted Au deposits are discrete hypogene and epigenetic masses usually hosted in a fault zone, breccia mass, or lithologic bed or unit.

沉积金矿床的矿体是一些不连续的内生或后生地质体,通常赋存于断裂带、角砾体或层(性单位)。

The extrusive rock unit includes basalt, andesite, boninite and albitite as well as breccia and tuff.

喷出岩单由玄武岩组成，还包括安岩、玻安岩、钠长岩以及角砾岩、凝灰岩等。

The first rock is mainly andesite clinkering agglomerate, andesite breccia, dacite breccia, rhyolite breccia and rhyolite clinkering tuff.

正常火碎屑岩亚类岩石类型主要为安质熔结集块岩,安质、英安质及纹质火角砾岩以及纹质熔结凝灰岩。

A new image shows possible "megabreccia" along the center of Mars's Coprates Chasma, a major trough in the Valles Marineris canyon system.

一种新的图像显示“巨形角砾岩”可能临近火星科普雷茨峡谷的中心，主要穿过瓦勒斯马里纳里斯峡谷。

Orebodies in sedirmentary rock hosted Au deposits are discrete hypogene and epigenetic masses usually hosted in a fault zone, breccia mass, or lithologic bed or unit.

积岩金矿床的矿体是一些连续的内生或后生地质体,通常赋存于断裂带、角砾岩体或岩层(岩性单位)中。

The extrusive rock unit includes basalt, andesite, boninite and albitite as well as breccia and tuff.

喷出岩单由玄武岩组成，还包括安岩、玻安岩、钠长岩以及角砾岩、凝灰岩等。

The first rock is mainly andesite clinkering agglomerate, andesite breccia, dacite breccia, rhyolite breccia and rhyolite clinkering tuff.

正常火碎屑岩亚类岩石类型主要为安质熔结集块岩,安质、英安质及纹质火角砾岩以及纹质熔结凝灰岩。

A new image shows possible "megabreccia" along the center of Mars's Coprates Chasma, a major trough in the Valles Marineris canyon system.

一种新的图像显示“巨形角砾岩”可能临近火星科普雷茨峡谷的中心，主要穿过瓦勒斯马里纳里斯峡谷。

Orebodies in sedirmentary rock hosted Au deposits are discrete hypogene and epigenetic masses usually hosted in a fault zone, breccia mass, or lithologic bed or unit.

积岩金矿床的矿体是一些连续的内生或后生地质体,通常赋存于断裂带、角砾岩体或岩层(岩性单位)中。

The extrusive rock unit includes basalt, andesite, boninite and albitite as well as breccia and tuff.

喷出单元不仅仅由玄武组成，还包括、玻、钠长以及角砾、凝灰等。

The first rock is mainly andesite clinkering agglomerate, andesite breccia, dacite breccia, rhyolite breccia and rhyolite clinkering tuff.

正常火碎屑亚类石类型主为质熔结集块,质、英质及纹质火角砾以及纹质熔结凝灰。

A new image shows possible "megabreccia" along the center of Mars's Coprates Chasma, a major trough in the Valles Marineris canyon system.

一种新的图像显示“巨形角砾”可能临近火星科普雷茨峡谷的中心，主瓦勒斯马里纳里斯峡谷系。

Orebodies in sedirmentary rock hosted Au deposits are discrete hypogene and epigenetic masses usually hosted in a fault zone, breccia mass, or lithologic bed or unit.

沉积金矿床的矿体是一些不连续的内生或后生地质体,通常赋存于断裂带、角砾体或层(性单位)中。

The extrusive rock unit includes basalt, andesite, boninite and albitite as well as breccia and tuff.

喷出岩单元不仅仅由玄武岩组成，还包括岩、玻岩、钠长岩以及砾岩、凝灰岩等。

The first rock is mainly andesite clinkering agglomerate, andesite breccia, dacite breccia, rhyolite breccia and rhyolite clinkering tuff.

正常碎屑岩亚类岩石类型主要为熔结集块岩,、英及纹砾岩以及纹熔结凝灰岩。

A new image shows possible "megabreccia" along the center of Mars's Coprates Chasma, a major trough in the Valles Marineris canyon system.

一种新的图像显示“巨形砾岩”可能临近星科普雷茨峡谷的中心，主要穿过瓦勒斯马里纳里斯峡谷系。

Orebodies in sedirmentary rock hosted Au deposits are discrete hypogene and epigenetic masses usually hosted in a fault zone, breccia mass, or lithologic bed or unit.

沉积岩金矿床的矿体是一些不连续的内生或后生地体,通常赋存于断裂带、砾岩体或岩层(岩性单位)中。

The extrusive rock unit includes basalt, andesite, boninite and albitite as well as breccia and tuff.

喷出单元不仅仅由玄武组成，还包括、玻、钠长及角、凝灰等。

The first rock is mainly andesite clinkering agglomerate, andesite breccia, dacite breccia, rhyolite breccia and rhyolite clinkering tuff.

正常火碎屑亚类石类型主要为质熔结集块,质、英质及纹质火角及纹质熔结凝灰。

A new image shows possible "megabreccia" along the center of Mars's Coprates Chasma, a major trough in the Valles Marineris canyon system.

一种新的图像显示“巨形角”可能临近火星科普雷茨峡谷的中心，主要穿过瓦勒斯马里纳里斯峡谷系。

Orebodies in sedirmentary rock hosted Au deposits are discrete hypogene and epigenetic masses usually hosted in a fault zone, breccia mass, or lithologic bed or unit.

沉积金矿床的矿体是一些不连续的内生或后生地质体,通常赋存于断裂带、角体或层(性单位)中。

The extrusive rock unit includes basalt, andesite, boninite and albitite as well as breccia and tuff.

喷出岩单元不玄武岩组成，还包括安岩、玻安岩、钠长岩以及角砾岩、凝灰岩等。

The first rock is mainly andesite clinkering agglomerate, andesite breccia, dacite breccia, rhyolite breccia and rhyolite clinkering tuff.

正常火碎屑岩亚类岩石类型主要为安质熔结集块岩,安质、英安质及纹质火角砾岩以及纹质熔结凝灰岩。

A new image shows possible "megabreccia" along the center of Mars's Coprates Chasma, a major trough in the Valles Marineris canyon system.

一种新的图像显示“巨形角砾岩”可能临近火星科普雷茨的中心，主要穿过瓦勒斯马里纳里斯系。

Orebodies in sedirmentary rock hosted Au deposits are discrete hypogene and epigenetic masses usually hosted in a fault zone, breccia mass, or lithologic bed or unit.

沉积岩金矿床的矿体是一些不连续的内生或后生地质体,通常赋存于断裂带、角砾岩体或岩层(岩性单位)中。