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関連する概念動画

Mechanism of Lamellipodia Formation01:31

Mechanism of Lamellipodia Formation

Cells migrating in response to external stimuli form lamellipodia, which are thin membrane protrusions supported by a mesh of linked, branched, or unbranched actin filaments. These actin filaments interact with myosin motor proteins, creating the dynamic actomyosin complex within the cytoskeleton. Contractility, or the ability to generate contractile stress, is inherent to the actomyosin complex. It helps cells detect the stiffness of the surrounding ECM and exert contractile force for...
Rapidly Varying Flow01:24

Rapidly Varying Flow

Rapidly varying flow (RVF) in open channels is characterized by abrupt changes in flow depth over a short distance, with the rate of depth change relative to distance often approaching unity. These flows are inherently complex due to their transient and multi-dimensional nature, making exact analysis difficult. However, approximate solutions using simplified models provide valuable insights into their behavior.Key Features of Rapidly Varying FlowRVF is commonly observed in scenarios involving...
Isothermal Processes01:21

Isothermal Processes

A thermodynamic process that occurs at constant temperature is called an isothermal process. Heat slowly flows into the system or out of the system to maintain thermal equilibrium. Processes involving phase changes like water evaporation into steam or freezing water into ice at a constant temperature are examples of Isothermal Processes.
An ideal gas can also undergo isothermal expansion or compression.
For example, consider 1 mole of an ideal gas inside an isolated cylinder at initial volume V...
Mechanism of Filopodia Formation01:39

Mechanism of Filopodia Formation

Filopodia are thin, actin-rich cellular protrusions that play an important role in many fundamental cellular functions. They vary in their occurrence, length, and positioning in different cell types, suggesting their diverse roles.
Their main function is to guide migrating cells during normal tissue morphogenesis or cancer metastasis by recognizing and making initial contacts with the extracellular matrix. However, they can also act as stationary cell anchors or help to establish communication...
Isochoric and Isobaric Processes01:21

Isochoric and Isobaric Processes

A thermodynamic process that occurs at constant volume is called an isochoric process. According to the first law of thermodynamics, heat supplied or removed from the system is partially utilized to perform work and change the internal energy of the system. However, in an isochoric process, the volume remains constant. Hence, the work done by the system is zero. Therefore, the exchange of heat changes the internal energy of the system only. 
Suppose 1000 g of water is heated from 40 degrees...
Speciation Rates01:07

Speciation Rates

Speciation can proceed at markedly different rates, and evolutionary biologists commonly describe these differences through the models of gradualism and punctuated equilibrium. Both patterns explain how new species arise, but they differ in the tempo and continuity of evolutionary change. In both cases, evolutionary change arises from heritable variation within populations, with natural selection often shaping traits that improve survival and reproduction under specific environmental conditions.

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関連する実験動画

Updated: Jul 12, 2026

Kinematic History of a Salient-recess Junction Explored through a Combined Approach of Field Data and Analog Sandbox Modeling
06:55

Kinematic History of a Salient-recess Junction Explored through a Combined Approach of Field Data and Analog Sandbox Modeling

Published on: August 5, 2016

ゆっくり広がる山脊における構造的プロセス

J C Mutter, J A Karson

    Science (New York, N.Y.)
    |July 31, 1992
    PubMed
    まとめ

    ゆっくり広がる中海の山脊は,急速に広がる山脊とは異なり,裂け目のある低地を示しています.

    科学分野:

    • 地質物理学とテクトニクス
    • 海洋地質学 海洋地質学
    • プレート・テクトニクス (プレート・テクトニクス)

    背景:

    • 中洋の山脊 (MORs) は,広がり速度に基づいて独特の特徴を示します.
    • ゆっくり広がるMOR (<35mm/yr) は,裂け目のある沈み込みと非対称性によって特徴付けられます.
    • 急速に広がるMORは,対称な火山建築を特徴としています.

    研究 の 目的:

    • ゆっくりと急速に広がる中海の山脊における対照的な地殻形成プロセスを調査する.
    • 脊のセグメンテーションにおける機械的変形とマグマ的プロセスの役割を決定する.

    主な方法:

    • ゆっくり広がる中海の山脊からの地震画像データの分析.
    • 地質学的特徴 (断層,地震,岩石の露出) を比較して,ゆっくりと急速に広がる山脊と,急速に広がる山脊を比較する.

    主要な成果:

    • ゆっくり広がる山脊は,深い地震,主要な正規断層,露出した下層の地殻岩で証明される重要な機械的変形を示しています.
    • ゆっくり広がる山脊におけるセグメンテーションは,主にマグマ的プロセスではなく,変形プロセスに関連しています.
    • 急速に広がる山脊は,対称で高い火山構造を示しています.

    さらに関連する動画

    Measuring Cell-Edge Protrusion Dynamics during Spreading using Live-Cell Microscopy
    05:50

    Measuring Cell-Edge Protrusion Dynamics during Spreading using Live-Cell Microscopy

    Published on: November 1, 2021

    Quantitative Analysis of Cell Edge Dynamics during Cell Spreading
    10:54

    Quantitative Analysis of Cell Edge Dynamics during Cell Spreading

    Published on: May 22, 2021

    関連する実験動画

    Last Updated: Jul 12, 2026

    Kinematic History of a Salient-recess Junction Explored through a Combined Approach of Field Data and Analog Sandbox Modeling
    06:55

    Kinematic History of a Salient-recess Junction Explored through a Combined Approach of Field Data and Analog Sandbox Modeling

    Published on: August 5, 2016

    Measuring Cell-Edge Protrusion Dynamics during Spreading using Live-Cell Microscopy
    05:50

    Measuring Cell-Edge Protrusion Dynamics during Spreading using Live-Cell Microscopy

    Published on: November 1, 2021

    Quantitative Analysis of Cell Edge Dynamics during Cell Spreading
    10:54

    Quantitative Analysis of Cell Edge Dynamics during Cell Spreading

    Published on: May 22, 2021

    結論:

    • 機械的変形は,急速に広がる山脊と比較して,ゆっくり広がる山脊で地殻形成においてより重要な役割を果たします.
    • ゆっくり広がる山脊のセグメンテーションは,本質的に変形プロセスと結びついています.
    • のセグメンテーションを理解することは,MORの進化を理解する鍵です.