glauconitic

简明释义

[ˌɡlɔːkəˈnɪtɪk][ˈɡlɔːkəˌnɪtɪk]

似海绿石的

含海绿石的

英英释义

Relating to or containing glauconite, a greenish mineral that is a form of clay and often found in marine sedimentary rocks.

与绿泥石有关或含有绿泥石,这是一种绿色矿物,属于粘土的一种,通常发现于海洋沉积岩中。

单词用法

glauconitic sandstone

绿泥石砂岩

glauconitic clay

绿泥石粘土

glauconitic sediment

绿泥石沉积物

glauconitic formation

绿泥石地层

同义词

greenish

绿色的

The glauconitic sandstone is often found in marine environments.

这种绿泥石砂岩通常出现在海洋环境中。

marine

海洋的

Glauconitic deposits indicate a low-energy depositional environment.

绿泥石沉积物表明低能量沉积环境。

sedimentary

沉积的

The greenish hue of the rock is due to the presence of glauconite.

岩石的绿色调是由于绿泥石的存在。

反义词

non-glauconitic

非绿泥石的

The non-glauconitic sediments are often found in deeper marine environments.

非绿泥石沉积物通常出现在更深的海洋环境中。

siliceous

硅质的

Siliceous rocks are commonly used in construction due to their durability.

硅质岩石因其耐用性而常用于建筑。

例句

1.In condensed sections, fossils and organic, phosphatic and glauconitic material tend to be concentrated compared with rapidly deposited sections that contain few fossils.

在凝缩剖面中,化石和有机物磷酸盐和海绿石质物质相对于几乎不含化石的快速沉积剖面而言,都趋向于被凝缩。

2.In condensed sections, fossils and organic, phosphatic and glauconitic material tend to be concentrated compared with rapidly deposited sections that contain few fossils.

在凝缩剖面中,化石和有机物磷酸盐和海绿石质物质相对于几乎不含化石的快速沉积剖面而言,都趋向于被凝缩。

3.The cower unit of the eagle is a well sorted lithic and glauconitic marine sandstone.

伊格尔砂岩的下部单元是分选良好的岩屑质和海相海绿石质。

4.The cower unit of the eagle is a well sorted lithic and glauconitic marine sandstone .

伊格尔砂岩的下部单元是分选良好的岩屑质和海相海绿石质。

5.The presence of glauconitic sandstones can be a sign of slow sedimentation rates.

出现绿泥石砂岩可能是沉积速率缓慢的迹象。

6.Geologists often analyze glauconitic layers to understand ancient oceanic conditions.

地质学家常常分析绿泥石层,以了解古代海洋条件。

7.In this area, the glauconitic clays are known for their high fertility.

在该地区,绿泥石粘土以其高肥力而闻名。

8.The sedimentary rock formation was rich in glauconitic minerals, indicating a marine environment.

该沉积岩层富含绿泥石矿物,表明其形成于海洋环境。

9.Drilling into glauconitic deposits can reveal valuable insights into past geological events.

钻探绿泥石沉积物可以揭示过去地质事件的宝贵见解。

作文

The study of geology often reveals fascinating insights into the Earth's history and composition. One notable aspect of sedimentary rocks is their mineral content, which can significantly impact both their formation and the environments in which they are found. Among these minerals, glauconitic (青绿石的) minerals are particularly interesting due to their unique characteristics and the clues they provide about past geological conditions. Glauconitic minerals are typically greenish in color and are primarily composed of the mineral glauconite, which is a type of mica that forms in marine environments. This mineral is often associated with sedimentary deposits that have undergone significant alteration over time.Understanding the formation of glauconitic (青绿石的) minerals can shed light on the conditions of ancient seas where they were deposited. These minerals typically form in shallow marine environments where organic matter accumulates and interacts with seawater. The presence of glauconitic (青绿石的) minerals in sedimentary layers indicates a specific set of environmental conditions, such as low sedimentation rates and a stable, warm climate conducive to the growth of marine life.In many regions, the occurrence of glauconitic (青绿石的) minerals is a key indicator of the geological history of the area. For example, in the Gulf Coast region of the United States, glauconitic (青绿石的) sediments are prevalent in certain formations, suggesting that these areas were once part of a shallow sea teeming with life. Geologists often analyze these sediments to reconstruct past environments and understand the evolution of marine ecosystems.Furthermore, glauconitic (青绿石的) minerals play an important role in the economic geology of certain regions. Their presence can indicate potential reservoirs of hydrocarbons, as these minerals often accumulate in areas rich in organic material. As such, the exploration for oil and gas frequently involves studying glauconitic (青绿石的) deposits to identify promising drilling sites.In addition to their geological significance, glauconitic (青绿石的) minerals also have implications for soil health and agriculture. Soils enriched with glauconitic (青绿石的) minerals can enhance nutrient availability and improve soil structure, making them more fertile and better suited for crop production. Farmers and agronomists may utilize this knowledge to optimize land use and enhance agricultural outputs.In conclusion, the study of glauconitic (青绿石的) minerals offers valuable insights into both the geological history of our planet and practical applications in various fields. From understanding ancient marine environments to exploring economic resources and enhancing agricultural practices, the significance of glauconitic (青绿石的) minerals cannot be overstated. As we continue to advance our knowledge of geology and mineralogy, the importance of these unique minerals will undoubtedly remain a focal point of research and exploration.

地质学的研究常常揭示出关于地球历史和组成的迷人见解。沉积岩的一个显著方面是它们的矿物成分,这可以显著影响它们的形成以及它们所处环境。在这些矿物中,glauconitic(青绿石的)矿物因其独特的特性和提供关于过去地质条件的线索而特别引人注目。Glauconitic矿物通常呈绿色,主要由青绿石矿物组成,这是一种在海洋环境中形成的云母类型。这种矿物通常与经历了显著变化的沉积物相联系。了解glauconitic(青绿石的)矿物的形成可以揭示出它们沉积时古代海洋的条件。这些矿物通常在有机物积累并与海水相互作用的浅海环境中形成。Glauconitic(青绿石的)矿物的存在表明了一系列特定的环境条件,例如低沉积速率和适合海洋生物生长的稳定温暖气候。在许多地区,glauconitic(青绿石的)矿物的出现是该地区地质历史的关键指标。例如,在美国的墨西哥湾沿岸地区,某些地层中普遍存在glauconitic(青绿石的)沉积物,表明这些地区曾经是充满生命的浅海的一部分。地质学家常常分析这些沉积物,以重建过去的环境并理解海洋生态系统的演变。此外,glauconitic(青绿石的)矿物在某些地区的经济地质中也发挥着重要作用。它们的存在可以指示潜在的碳氢化合物储层,因为这些矿物通常在富含有机物的区域积累。因此,石油和天然气的勘探通常涉及研究glauconitic(青绿石的)沉积物,以识别有希望的钻探地点。除了它们的地质意义外,glauconitic(青绿石的)矿物对土壤健康和农业也有影响。富含glauconitic(青绿石的)矿物的土壤可以增强养分的可用性并改善土壤结构,使其更肥沃,更适合作物生产。农民和农艺师可能利用这一知识来优化土地使用,提高农业产出。总之,研究glauconitic(青绿石的)矿物为我们提供了关于地球地质历史和各个领域实际应用的宝贵见解。从理解古代海洋环境到探索经济资源以及增强农业实践,glauconitic(青绿石的)矿物的重要性不容小觑。随着我们继续推进对地质学和矿物学的了解,这些独特矿物的重要性无疑将始终是研究和探索的焦点。