taphrogenesis

简明释义

英[tæf.rəʊ.dʒəˈnɛs.ɪs]美[tæf.roʊ.dʒəˈnɛs.ɪs]

断裂运动

英英释义

单词用法

同义词

反义词

例句

1.The structural framework, formed by Emei Taphrogenesis, controlled the sedimentation and diagenesis, thus more or less controlled the distribution of hydrocarbon in the area.

地裂运动形成的构造格局对沉积、成岩有一定的控制作用，进而在一定程度上控制了该区油气的分布。

2.Permian, Permian and Triassic were the outset, peak and close stages of the Emei Taphrogenesis, respectively.

二叠纪前为地裂运动伊始期； 二纪为地裂运动高峰期；三叠纪为地裂运动衰退期。

3.The structural framework, formed by Emei Taphrogenesis, controlled the sedimentation and diagenesis, thus more or less controlled the distribution of hydrocarbon in the a...

地裂运动形成的构造格局对沉积、成岩有一定的控制作用，进而在一定程度上控制了该区油气的分布。

4.The structural framework, formed by Emei Taphrogenesis, controlled the sedimentation and diagenesis, thus more or less controlled the distribution of hydrocarbon in the area.

地裂运动形成的构造格局对沉积、成岩有一定的控制作用，进而在一定程度上控制了该区油气的分布。

5.The concept of taphrogenesis is crucial for reconstructing ancient ecosystems based on fossil evidence.

在基于化石证据重建古生态系统时，taphrogenesis的概念至关重要。

6.Recent findings in taphrogenesis have changed our perspective on how quickly certain organisms can fossilize.

关于taphrogenesis的最新发现改变了我们对某些生物化石化速度的看法。

7.Researchers are exploring the role of sedimentation in taphrogenesis to better understand fossil preservation.

研究人员正在探讨沉积作用在taphrogenesis中的作用，以更好地理解化石保存。

8.Understanding taphrogenesis can help paleontologists determine the conditions under which fossils were formed.

理解taphrogenesis可以帮助古生物学家确定化石形成的条件。

9.The study of taphrogenesis reveals how environmental factors influence the fossilization process.

对taphrogenesis的研究揭示了环境因素如何影响化石化过程。

作文

The concept of taphrogenesis refers to the processes that lead to the formation and alteration of sedimentary rocks through various geological mechanisms. Understanding this term is crucial for geologists and paleontologists alike, as it helps them comprehend how sediments are deposited, transformed, and ultimately fossilized. In essence, taphrogenesis encompasses the entire journey of sediment from its initial deposition to its final state as part of the rock record. This journey involves several stages, including transportation, compaction, cementation, and diagenesis.To illustrate the significance of taphrogenesis, consider the example of a river delta. As rivers flow towards the ocean, they carry with them a variety of sediments — clay, silt, and sand. When these sediments reach the delta, they begin to settle and accumulate. Over time, the weight of the overlying materials compresses the sediments below, initiating the process of compaction. During this stage, water is expelled from the pore spaces between the sediment grains, leading to an increase in density.Following compaction, the next phase in taphrogenesis is cementation. This process occurs when minerals precipitate from groundwater and fill the spaces between sediment grains, effectively ‘gluing’ them together. Common minerals involved in cementation include calcite, quartz, and hematite. The result is a solid rock formation that retains the original characteristics of the sediment while also incorporating new mineralogical properties.Diagenesis, the final stage of taphrogenesis, refers to the physical and chemical changes that occur in sediments after their initial lithification. This can involve further compaction, recrystallization of minerals, or even the introduction of new materials through hydrothermal fluids. Diagenesis plays a critical role in determining the porosity and permeability of sedimentary rocks, which are essential factors in natural resource exploration, particularly in the fields of petroleum and groundwater.Moreover, understanding taphrogenesis is vital for reconstructing past environments and ecosystems. By studying the sedimentary record, scientists can infer the conditions under which the sediments were deposited, providing insights into ancient climates, sea levels, and biological activity. For instance, the presence of certain fossils within a sedimentary layer can indicate specific environmental conditions, such as whether the area was once a marine or terrestrial habitat.In conclusion, taphrogenesis is a fundamental concept in geology that encompasses the processes involved in the formation and alteration of sedimentary rocks. From the initial deposition of sediments to their transformation into solid rock, each stage of taphrogenesis provides valuable information about Earth’s history and the dynamic processes that shape our planet. As we continue to explore and study these geological processes, our understanding of the Earth’s past, present, and future will only deepen, highlighting the importance of taphrogenesis in the broader context of geological sciences.

“taphrogenesis”一词指的是通过各种地质机制导致沉积岩的形成和变化的过程。理解这个术语对地质学家和古生物学家来说至关重要，因为它帮助他们理解沉积物是如何沉积、转变并最终化石化的。从本质上讲，taphrogenesis涵盖了沉积物从最初沉积到最终作为岩石记录一部分的整个旅程。这个旅程包括几个阶段，包括运输、压实、胶结和成岩。为了说明taphrogenesis的重要性，可以考虑河口三角洲的例子。当河流流向海洋时，它们携带着各种沉积物——粘土、淤泥和沙子。当这些沉积物到达三角洲时，它们开始沉降和积累。随着时间的推移，上覆材料的重量压缩下面的沉积物，启动了压实过程。在这个阶段，水从沉积颗粒之间的孔隙中被排出，导致密度增加。在压实之后，taphrogenesis的下一个阶段是胶结。当矿物从地下水中沉淀并填满沉积颗粒之间的空间时，这一过程发生，有效地将它们‘粘合’在一起。参与胶结的常见矿物包括方解石、石英和赤铁矿。结果是一个固体岩石形成，它保留了沉积物的原始特征，同时也融入了新的矿物特性。成岩是taphrogenesis的最后阶段，指的是沉积物在初始固化后发生的物理和化学变化。这可能涉及进一步的压实、矿物的再结晶，或甚至通过热液流体引入新材料。成岩在决定沉积岩的孔隙度和渗透性方面发挥着关键作用，这些都是自然资源勘探中至关重要的因素，特别是在石油和地下水领域。此外，理解taphrogenesis对于重建过去的环境和生态系统至关重要。通过研究沉积记录，科学家可以推断沉积物沉积时的条件，从而提供对古代气候、海平面和生物活动的洞察。例如，某一沉积层中存在特定化石可以指示该区域曾经是海洋或陆地栖息地。总之，taphrogenesis是地质学中的一个基本概念，涵盖了与沉积岩的形成和变化有关的过程。从沉积物的初始沉积到它们转变为固体岩石的过程，taphrogenesis的每个阶段都提供了关于地球历史和塑造我们星球的动态过程的宝贵信息。随着我们继续探索和研究这些地质过程，我们对地球的过去、现在和未来的理解将不断加深，突显了taphrogenesis在更广泛的地质科学背景中的重要性。